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Sample records for map pacific ocean

  1. Ocean dynamics and thermodynamics in the tropical Indo- Pacific region

    E-Print Network [OSTI]

    Drushka, Kyla

    2011-01-01

    Pacific Oceans . . . . . . . . . . . . . . . . . . . . . . . . . . . . .in the eastern tropical Pacific Ocean associated with thethe western equatorial Pacific Ocean. J. Geophys. Res. , 96,

  2. Pelagic Polychaetes of the Pacific Ocean

    E-Print Network [OSTI]

    Dales, K Phillips

    1957-01-01

    Polyc'kaetes of the Pacific Ocean CLAPARtDE,E. 1868. LesPolyc'haetes of the Pacific Ocean KINBERG, J. G. H. 1866.Polyc'kaetes of the Pacific Ocean TREADWELL, A. L. 1906.

  3. Heat Content Changes in the Pacific Ocean

    E-Print Network [OSTI]

    Frandsen, Jannette B.

    Heat Content Changes in the Pacific Ocean The Acoustic Thermometry of Ocean Cli- mate (ATOC assimilating ocean observations and changes expected from surface heat fluxes as measured by the daily National are a result of advection of heat by ocean currents. We calculate that the most likely cause of the discrepancy

  4. Distribution of anthropogenic CO2 in the Pacific Ocean

    E-Print Network [OSTI]

    Distribution of anthropogenic CO2 in the Pacific Ocean C. L. Sabine,1 R. A. Feely,2 R. M. Key,3 J] This work presents an estimate of anthropogenic CO2 in the Pacific Ocean based on measurements from the WOCE tracers; 9355 Information Related to Geographic Region: Pacific Ocean; KEYWORDS: Pacific Ocean

  5. Open ocean DMS air/sea fluxes over the eastern South Pacific Ocean

    E-Print Network [OSTI]

    Marandino, C. A; De Bruyn, W. J; Miller, S. D; Saltzman, E. S

    2009-01-01

    over the North Pacific Ocean, J. Geophys. Res. - Atmos. ,air/sea fluxes over S. Pacific Ocean References Asher, W.in the equa- torial Pacific Ocean ( 1982 to 1996): Evidence

  6. A synthesis of marine predator migrations, distribution, species overlap, and use of Pacific Ocean Exclusive Economic Zones

    E-Print Network [OSTI]

    Harrison, Autumn-Lynn

    2012-01-01

    North Pacific Ocean . . . . . . . . . . . . . . . . . . . .month in the North Pacific Ocean . . . . . . . . . . . .tracked in the Pacific Ocean during 2002-2009. Adapted from

  7. Eddy correlation measurements of the air/sea flux of dimethylsulfide over the North Pacific Ocean

    E-Print Network [OSTI]

    Marandino, C. A; De Bruyn, W. J; Miller, S. D; Saltzman, E. S

    2007-01-01

    radon over the northeast Pacific Ocean, J. Atmos. Chem. , 6,in the equatorial Pacific Ocean (1982 to 1996): Evidence ofover the northeast Pacific Ocean, J. Atmos. Chem. , Bates,

  8. Intermediate-depth circulation of the Indian and South Pacific Oceans measured by autonomous floats

    E-Print Network [OSTI]

    Davis, Russ E

    2005-01-01

    circulation of the Pacific Ocean: Flow patterns, tracers,the Indian and South Pacific Oceans Measured by Autonomousthe tropical and South Pacific Ocean and 228 were deployed

  9. Trophic understanding of tunas of the Southwest Pacific Ocean

    E-Print Network [OSTI]

    Hawai'i at Manoa, University of

    Trophic understanding of tunas of the Southwest Pacific Ocean WEALTH FROM OCEANS FLAGSHIP Jock of tunas of the Southwest Pacific Ocean| JWY3 | Thunnus tonggol Thunnus obesus Thunnus albacares Thunnus of the Southwest Pacific Ocean| JWY4 | Species SCA DR SIA SFA Thunnus alalunga + + + 0 Thunnus albacares + + + 0

  10. HEAT STORAGE AND ADVECTION IN THE NORTH PACIFIC OCEAN

    E-Print Network [OSTI]

    Luther, Douglas S.

    HEAT STORAGE AND ADVECTION IN THE NORTH PACIFIC OCEAN A DISSERTATION SUBMITTED TO THE GRADUATE maintaining the seasonal heat storage in the 0 to 250 meter surface layer of the North Pacific Ocean. Approximately 140,000 bathy- thermograph observations taken in the Pacific Ocean from 10° South latitude to 70

  11. Scholarly Paper Coupled Instability in the Equatorial Pacific Ocean

    E-Print Network [OSTI]

    Maryland at College Park, University of

    Scholarly Paper Coupled Instability in the Equatorial Pacific Ocean Hua Chen Advisor: Raghu's a cycle or an event depends on the mean state of equatorial Pacific Ocean, which is influenced by mean problem in the equatorial Pacific ocean. The control run with a coupling coefficient 0.4 and relatively

  12. DEEP MAXIMA OF PHOTOSYNTHETIC CHLOROPHYLL IN THE PACIFIC OCEAN

    E-Print Network [OSTI]

    DEEP MAXIMA OF PHOTOSYNTHETIC CHLOROPHYLL IN THE PACIFIC OCEAN E. L. VENRICK, J. A. MCGOWAN, AND A Pacific Ocean show that during most of the year the maximum concentrations of chlorophyll occur below in the world's oceans. There are several thousands of these measurements in the Pacific. Most

  13. Pacific Ocean Contribution to the Asymmetry in Eastern Indian Ocean Variability CAROLINE C. UMMENHOFER*

    E-Print Network [OSTI]

    Ummenhofer, Caroline C.

    Pacific Ocean Contribution to the Asymmetry in Eastern Indian Ocean Variability CAROLINE C is restricted to the Indian or Pacific Ocean only, support the interpretation of forcing mechanisms for large Indian Ocean atmospheric forcing versus remote influences from Pacific wind forcing: low events develop

  14. TELECONNECTIONS BETWEEN NORTHEASTERN PACIFIC OCEAN AND THE GULF OF MEXICO AND NORTHWESTERN ATLANTIC OCEAN

    E-Print Network [OSTI]

    TELECONNECTIONS BETWEEN NORTHEASTERN PACIFIC OCEAN AND THE GULF OF MEXICO AND NORTHWESTERN ATLANTIC-scale interactions in the tropical Pacific Ocean, especially, processes associated with the EI Nino phenomena. He has of ocean temperatures. He suggests that an anomalously high heat supply in the equatorial Pacific

  15. Extrapolating Oceanic Age Distributions: Lessons from the Pacific Region

    E-Print Network [OSTI]

    Extrapolating Oceanic Age Distributions: Lessons from the Pacific Region David B. Rowley Department plate reconstructions. An area equal in size to the Pacific Basin oceanic lithosphere must-mail: rowley@geosci.uchicago.edu) A B S T R A C T Extrapolation of the age distribution of oceanic lithosphere

  16. Mode coherence at megameter ranges in the North Pacific Ocean

    E-Print Network [OSTI]

    Wage, Kathleen

    Mode coherence at megameter ranges in the North Pacific Ocean Kathleen E. Wage, Matthew A and the Acoustical Society of America. #12;Mode coherence at megameter ranges in the North Pacific Ocean Kathleen E Thermometry of Ocean Climate ATOC and Alternate Source Test AST experiments. Vertical line arrays at Hawaii

  17. Northerly surface wind events over the eastern North Pacific Ocean : spatial distribution, seasonality, atmospheric circulation, and forcing

    E-Print Network [OSTI]

    Taylor, Stephen V.

    2006-01-01

    atmosphere over the eastern Pacific Ocean in summer, volumeover the eastern North Pacific Ocean: Spatial distribution,winds over the eastern North Pacific Ocean in spring and

  18. Examining Management Issues for Incidentally Caught Species in Highly Migratory Species Fisheries in the Western and Central Pacific Ocean

    E-Print Network [OSTI]

    Chan, Valerie Ann

    2014-01-01

    dynamics in the central Pacific Ocean, 1952- 1998. II. Afishing for tunas in the Pacific Ocean. Ecology and Societywestern and central north Pacific Ocean. ISC. 2013a. Stock

  19. Alkyl nitrate (C 1 -C 3 ) depth profiles in the tropical Pacific Ocean

    E-Print Network [OSTI]

    Dahl, E. E; Yvon-Lewis, S. A; Saltzman, E. S

    2007-01-01

    Experiment (WOCE), vol. 2, Pacific Ocean DRAFT, edited by M.over the equatorial Pacific Ocean during SAGA 3, J. Geophys.the troposphere over the Pacific Ocean during PEM- Tropics A

  20. Tropical Pacific nutrient dynamics in the modern and pleistocene ocean : insights from the nitrogen isotope system

    E-Print Network [OSTI]

    Rafter, Patrick Anthony

    2009-01-01

    eastern equatorial Pacific Ocean during the past 3 M.Y. ,in the western tropical Pacific Ocean in the Holocene epoch,eastern tropical North Pacific Ocean, Mar. Chem. , 3, 271–

  1. Boundary scavenging in the Pacific Ocean: a comparison of 10Be and 231Pa

    E-Print Network [OSTI]

    Anderson, RF; Lao, Y; Broecker, WS; Trumbore, SE; Hofmann, HJ; Wolfli, W

    1990-01-01

    sedi- ments of the Pacific Ocean, Geochim. Cosmochim. Actadust input to the North Pacific Ocean during the past 30,000rates within the Pacific Ocean, in: Dynamic Processes in the

  2. Asian anthropogenic lead contamination in the North Pacific Ocean as evidenced by stable lead isotopic compositions

    E-Print Network [OSTI]

    Zurbrick, Cheryl Marie

    2014-01-01

    and North Central Pacific Ocean. Deep Sea Res. Part II Top.Lead Within the Northwest Pacific Ocean Evidenced by Leadventilation flux of the Pacific Ocean. J. Geophys. Res. 106(

  3. CURRENT SKIPJACK OCEANOGRAPHY CRUISES IN EASTERN TROPICAL PACIFIC OCEAN

    E-Print Network [OSTI]

    CURRENT SKIPJACK OCEANOGRAPHY CRUISES IN EASTERN TROPICAL PACIFIC OCEAN F. Williams A series of skipjack oceanography cruises is planned for two offshore areas in the eastern tropical Pacific Ocean October 23 and arrived in Honolulu November 29; and the David Starr Jordan (Fishery-Oceanography C en t e

  4. Input of 129 I into the western Pacific Ocean resulting

    E-Print Network [OSTI]

    Buesseler, Ken

    Input of 129 I into the western Pacific Ocean resulting from the Fukushima nuclear event S. J characterization of the input of 129 I into the Pacific Ocean resulting from the 2011 Fukushima nuclear accident at the Fuku- shima Daiichi nuclear power plant that caused the release of radioactive elements

  5. The distinct behaviors of Pacific and Indian Ocean warm pool properties on seasonal and interannual time scales

    E-Print Network [OSTI]

    Kim, Seon Tae; Yu, Jin-Yi; Lu, Mong-Ming

    2012-01-01

    the tropical Indian and Pacific Ocean regions, Mon. WeatherIndian Ocean and in the Pacific Ocean, J. Ocean Univ. China,KIM ET AL. : PACIFIC AND INDIAN OCEAN WARM POOL Rayner, N.

  6. Ocean Observatories Initiative: Pacific Northwest The Endurance Array

    E-Print Network [OSTI]

    Kurapov, Alexander

    Ocean Observatories Initiative: Pacific Northwest The Endurance Array The processes that shape. The Ocean Observatories Initiative (OOI) will build a 25­30 year laboratory on the seafloor, in the water column, and at the ocean surface. It will make available novel platforms for oceanographic discovery

  7. MORPHOMETRIC VARIATION OF PACIFIC OCEAN PERCH, SEBASTES ALUTUS, OFF WESTERN NORTH AMERICA

    E-Print Network [OSTI]

    MORPHOMETRIC VARIATION OF PACIFIC OCEAN PERCH, SEBASTES ALUTUS, OFF WESTERN NORTH AMERICA JAY C. QUAST' ABSTRACT Pacific ocean perch. Sebastes alufus, vary in body form over the eastern Pacific Ocean be phenotypic. Pacific ocean perch, Sebastes alutus, a commer- cially important rockfish IScorpaenidae

  8. Recent Bottom Water Warming in the Pacific Ocean* GREGORY C. JOHNSON

    E-Print Network [OSTI]

    Laughlin, Robert B.

    Recent Bottom Water Warming in the Pacific Ocean* GREGORY C. JOHNSON NOAA/Pacific Marine) ABSTRACT Decadal changes of abyssal temperature in the Pacific Ocean are analyzed using high-quality, full the source of bottom water for the Pacific Ocean, which enters the main deep basins of this ocean southeast

  9. Trophic understanding of tunas of the Southwest Pacific Ocean

    E-Print Network [OSTI]

    Hawai'i at Manoa, University of

    Working Group 3) · Trophic ecology · Chemical indicators · Bioenergetics · Niche separation · Climate indicators Bioenergetics Niche separation Climate change 7 | Trophic understanding of tunas of the Southwest of tunas of the Southwest Pacific Ocean Trophic ecology Chemical indicators Bioenergetics Niche separation

  10. Relationships between Pacific and Atlantic ocean sea surface temperatures and U.S. streamflow variability

    E-Print Network [OSTI]

    Piechota, Thomas C.

    Relationships between Pacific and Atlantic ocean sea surface temperatures and U.S. streamflow March 2006; published 19 July 2006. [1] An evaluation of Pacific and Atlantic Ocean sea surface by an interdecadal-temporal evaluation for the Pacific (Atlantic) Ocean based on the phase of the Pacific Decadal

  11. Closure of the global overturning circulation through the Indian, Pacific and Southern Oceans: schematics and transports

    E-Print Network [OSTI]

    Talley, Lynne D.

    internal diapycnal transformation in the deep Indian and Pacific Oceans. All three northern-source Deep and Pacific Oceans; only 0.1 PW is gained at the surface in the Southern Ocean. Thus, while an adiabatic model full participation of the diffusive Indian and Pacific Oceans, with a basin-averaged diffusivity

  12. Journal of Oceanography, Vol. 60, pp. 163 to 188, 2004 Pacific Ocean,

    E-Print Network [OSTI]

    Xiu, Peng

    163 Journal of Oceanography, Vol. 60, pp. 163 to 188, 2004 Keywords: Pacific Ocean, decadal. Decadal-Scale Climate and Ecosystem Interactions in the North Pacific Ocean ARTHUR J. MILLER 1 *, FEI CHAI variations in the Pacific Ocean wield a strong influence on the oceanic ecosystem. Two dominant patterns

  13. Mapping and Assessment of the United States Ocean Wave Energy...

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Mapping and Assessment of the United States Ocean Wave Energy Resource Mapping and Assessment of the United States Ocean Wave Energy Resource This report describes the analysis and...

  14. Impacts of Pacific and Indian Ocean Coupling on Wintertime Tropical Intraseasonal Oscillation: A Basin-Coupling CGCM Study

    E-Print Network [OSTI]

    Weng, Shu-Ping; Yu, Jin-Yi

    2010-01-01

    the central Indian and Pacific oceans. We notice from FigureIP) Run, (c) the Pacific Ocean (PO) Run, and (d) the Indiantropical Indian and Pacific Oceans. Journal of Climate 10:

  15. Radiocarbon and stable carbon isotope compositions of organic compound classes in sediments from the NE Pacific and Southern Oceans

    E-Print Network [OSTI]

    Wang, XC; Druffel, ERM

    2001-01-01

    in the deep Northeast Pacific Ocean. Geophys. Res. Lett. 23,sediment of the Northeast Pacific Ocean. Geochim. Cosmochim.in the eastern North Pacific Ocean. J. Geophys. Res. 103,

  16. Bomb-test 90Sr in Pacific and Indian Ocean surface water as recorded by banded corals

    E-Print Network [OSTI]

    Toggweiler, JR; Trumbore, S

    1985-01-01

    the eastern tropical Pacific Ocean, Geophys. Res. Lett. 8,Bomb tritium in the Pacific Ocean, J. Geophys. Res. 80,of tritium in the Pacific Ocean, J. Phys. Oceanogr. II, 3,

  17. Late Quaternary variability of sedimentary nitrogen isotopes in the eastern South Pacific Ocean

    E-Print Network [OSTI]

    Demouchy, Sylvie

    Late Quaternary variability of sedimentary nitrogen isotopes in the eastern South Pacific Ocean), Late Quaternary variability of sedimentary nitrogen isotopes in the eastern South Pacific Ocean) in the water columns of the Arabian Sea (AS) and the eastern North and South Pacific oceans (ENP; ESP) holds

  18. An optimizing reduced order FDS for the tropical Pacific Ocean reduced gravity model

    E-Print Network [OSTI]

    Aluffi, Paolo

    An optimizing reduced order FDS for the tropical Pacific Ocean reduced gravity model Zhendong Luoa) for the tropical Pacific Ocean reduced gravity model. Ensembles of data are compiled from transient solutions computed from the discrete equation system derived by FDS for the tropical Pacific Ocean reduced gravity

  19. Intermediate Zonal Jets in the Tropical Pacific Ocean Observed by Argo Floats* SOPHIE CRAVATTE

    E-Print Network [OSTI]

    Boyer, Edmond

    Intermediate Zonal Jets in the Tropical Pacific Ocean Observed by Argo Floats* SOPHIE CRAVATTE´veloppement, LEGOS, Toulouse, France WILLIAM S. KESSLER National Oceanic and Atmospheric Administration/Pacific Argo float data in the tropical Pacific Ocean during January 2003­August 2011 are analyzed to obtain

  20. North Pacific Gyre Oscillation links ocean climate and ecosystem E. Di Lorenzo,1

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    North Pacific Gyre Oscillation links ocean climate and ecosystem change E. Di Lorenzo,1 N Pacific Gyre Oscillation links ocean climate and ecosystem change, Geophys. Res. Lett., 35, L08607, doi:10 to explain physical and biological fluctuations in the Northeast Pacific Ocean [Lynn et al., 1998; Lavaniegos

  1. 1 Drivers of the projected changes to the Pacific Ocean 2 equatorial circulation

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    1 Drivers of the projected changes to the Pacific Ocean 2 equatorial circulation 3 A. Sen Gupta,1 A), 29 Drivers of the projected changes to the Pacific Ocean equatorial 30 circulation, Geophys. Res. Lett., 39, LXXXXX, doi:10.1029/ 31 2012GL051447. 32 1. Introduction 33 [2] The equatorial Pacific Ocean

  2. Intraseasonal Eastern Pacific Precipitation and SST Variations in a GCM Coupled to a Slab Ocean Model

    E-Print Network [OSTI]

    Maloney, Eric

    Intraseasonal Eastern Pacific Precipitation and SST Variations in a GCM Coupled to a Slab Ocean-Schubert convection to a slab ocean model (SOM) improves the simulation of eastern Pacific convection during and ocean make eastern Pacific low-level circulation anomalies more complex in the SOM simulation than

  3. The depth of the tropical Pacific Ocean's warm surface layer shrank during the last three

    E-Print Network [OSTI]

    Yanik, Mehmet Fatih

    The depth of the tropical Pacific Ocean's warm surface layer shrank during the last three decades Pacific Ocean, off an island in Palau. They analysed the ratio of nitrogen and carbon isotopes.1029/2010GL044867 (2010) OceanOgraphy Cold water rising in the Pacific DrUg DeVeLOpMenT Worm surgery on a chip

  4. Interactions between the Indonesian Throughflow and circulations in the Indian and Pacific Oceans

    E-Print Network [OSTI]

    Jensen, Tommy

    Interactions between the Indonesian Throughflow and circulations in the Indian and Pacific Oceans with the Indonesian Throughflow (IT), particularly concerning subsurface currents in the Pacific Ocean, are studied model (LOM), both confined to the Indo-Pacific basin; and a global, ocean general circulation model

  5. Eddy mean flow decomposition and eddy diffusivity estimates in the tropical Pacific Ocean

    E-Print Network [OSTI]

    Eddy mean flow decomposition and eddy diffusivity estimates in the tropical Pacific Ocean: 2] Eddy diffusivity of the surface velocity field in the tropical Pacific Ocean was estimated using diffusivity estimates in the tropical Pacific Ocean: 2. Results, J. Geophys. Res., 107(C10), 3154, doi:10

  6. MODEL OF THE .MIGRATION OF ALBACORE IN THE NORTH PACIFIC OCEAN

    E-Print Network [OSTI]

    MODEL OF THE .MIGRATION OF ALBACORE IN THE NORTH PACIFIC OCEAN .By TAMIO OTSU and RICHARD N. UCHIDA of the migration of albacore in the North Pacific Ocean has been developed. This model is consistent with the hypothesis that there is a single population of albacore in the North Pacific Ocean. . The model depicts

  7. A deeper respired carbon pool in the glacial equatorial Pacific Ocean L.I. Bradtmiller a,

    E-Print Network [OSTI]

    Sachs, Julian P.

    A deeper respired carbon pool in the glacial equatorial Pacific Ocean L.I. Bradtmiller a, , R in paleoceanography. We present evidence from ten equatorial Pacific Ocean sediment cores to show that the deep Pacific Ocean likely stored more carbon during the last glacial period than the Holocene

  8. Ocean mixed layer processes in the Pacific Decadal Oscillation in coupled general circulation models

    E-Print Network [OSTI]

    Qiu, Bo

    Ocean mixed layer processes in the Pacific Decadal Oscillation in coupled general circulation to be larger for CGCMs with a larger ocean heat transport in the region. Keywords Pacific Decadal Oscillation Á. 1994a, b; Zhanget al. 1996), ocean-atmosphere interactions over the North Pacific (e.g., Latif

  9. Effects of correcting salinity with altimeter measurements in an equatorial Pacific ocean model

    E-Print Network [OSTI]

    van Leeuwen, Peter Jan

    Effects of correcting salinity with altimeter measurements in an equatorial Pacific ocean model in a tropical Pacific ocean model run for the period 1993­1997. Salinity and temperature corrections salinity with altimeter measurements in an equatorial Pacific ocean model, J. Geophys. Res., 107(C12), 8001

  10. Evolution of Tidal Amplitudes in the Eastern Pacific Ocean

    E-Print Network [OSTI]

    Hickey, Barbara

    amplitudes may impact ocean mixing, nutrient supply, primary production, fisher- ies, and coastal erosion [Flick et al., 2003]. To understand the causes of the evolution of coastal tides, it is necessary) and semidiurnal (M2) constituents in the Eastern Pacific from Chile to Alaska (33ºS to 60ºN latitude). The only

  11. Quaternary Science Reviews 20 (2001) 15611576 Millennial scale climate variability of the northeast Pacific Ocean and

    E-Print Network [OSTI]

    Kurapov, Alexander

    2001-01-01

    of the northeast Pacific Ocean and northwest North America based on radiolaria and pollen N.G. Pisiasa, *, A in the Northeast Pacific and the northwestern United States. 2. Study region 2.1. Ocean climate and biota.C. Mixa , L. Heusserb a College of Oceanic and Atmospheric Sciences, Oregon State University, 104 Ocean

  12. Radiocarbon in particulate matter from the eastern sub-arctic Pacific Ocean; evidence of a source of terrestrial carbon to the deep sea.

    E-Print Network [OSTI]

    Druffel, Ellen R M; Honju, Susumu; Griffin, Sheila; Wong, C S

    1986-01-01

    in the sub-Arctic Pacific Ocean: Inter- natl North PacificSalmon of the North Pacific Ocean-Part II-Review of theproduced carbon-14 by the Pacific Ocean: Ph D dissert, Univ

  13. Variation of the Thermohaline Structure in the Western Equatorial Pacific Upper Ocean

    E-Print Network [OSTI]

    Luther, Douglas S.

    Variation of the Thermohaline Structure in the Western Equatorial Pacific Upper Ocean;Abstract Processes which control the upper ocean thermohaline structure in the western equa- torial Pacific forcing data have indicated that the thick isothermal layer in the western equatorial Pacific is found

  14. Reduced Order Modeling of the Upper Tropical Pacific Ocean Model Using Proper Orthogonal Decomposition

    E-Print Network [OSTI]

    Aluffi, Paolo

    Reduced Order Modeling of the Upper Tropical Pacific Ocean Model Using Proper Orthogonal of a large-scale upper ocean circulation in the tropic Pacific domain. We construct different POD models-scale seasonal variability of the tropic Pacific obtained by the original model is well captured by a low

  15. From the subtropics to the central equatorial Pacific Ocean: Neodymium isotopic composition and rare earth element

    E-Print Network [OSTI]

    Boyer, Edmond

    From the subtropics to the central equatorial Pacific Ocean: Neodymium isotopic composition, and S. Cravatte (2013), From the subtropics to the central equatorial Pacific Ocean: Neodymium isotopic waters (112 samples) in the Southern Tropical Pacific. The relatively detailed picture of these tracer

  16. Status Assessment of Laysan and Black-Footed Albatrosses, North Pacific Ocean, 19232005

    E-Print Network [OSTI]

    Schweik, Charles M.

    of Laysan and black-footed albatrosses. Photograph taken by Eric VanderWerf, Pacific Rim Conservation. #12Status Assessment of Laysan and Black-Footed Albatrosses, North Pacific Ocean, 1923­2005 Scientific;Status Assessment of Laysan and Black-Footed Albatrosses, North Pacific Ocean, 1923­2005 By Javier A

  17. Assessment of the amount of cesium-137 released into the Pacific Ocean after the Fukushima accident

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    Assessment of the amount of cesium-137 released into the Pacific Ocean after the Fukushima accident into the Pacific Ocean after the Fukushima accident and analysis of its dispersion in Japanese coastal waters, J into the ocean from the Fukushima Daiichi nuclear power plant (NPP) after the accident in March 2011 and to gain

  18. INTEGRITY OF SCHOOLS OF SKIPJACK TUNA, KATSUWONUS PELAMIS, IN THE EASTERN PACIFIC OCEAN,

    E-Print Network [OSTI]

    INTEGRITY OF SCHOOLS OF SKIPJACK TUNA, KATSUWONUS PELAMIS, IN THE EASTERN PACIFIC OCEAN Pacific yellowfin [(Thunnus albacares)] and the Pac.ific-wide skipjack [(KatS'Uwonus pelamis

  19. THE EARLY LIFE HISTORY OF SKIPJACK TUNA, Katsuwonus pelamis, IN THE PACIFIC OCEAN

    E-Print Network [OSTI]

    THE EARLY LIFE HISTORY OF SKIPJACK TUNA, Katsuwonus pelamis, IN THE PACIFIC OCEAN HOWARD O. YOSHIDA, Katsuwonus pelamis, were landed in the eastern Pacific (Inter-American Tropical Tuna Commis- sion, 1970

  20. Seasonal and interannual variability of ocean color and composition of phytoplankton communities in the North Atlantic, Equatorial Pacific and South Pacific.

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    Seasonal and interannual variability of ocean color and composition of phytoplankton communities in the North Atlantic, Equatorial Pacific and South Pacific. By : Yves Dandonneaua , Pierre-Yves Deschampsb ­ Picoplankton ­ Seasonal variations ­ Variability ­ Oceanic provinces ) Contact : Yves DANDONNEAU LODYC

  1. GEOPHYSICAL RESEARCH LETTERS, VOL. 0, NO. 0, PAGES 0-0, M 0, 2001 On the Pacific Ocean regime shift

    E-Print Network [OSTI]

    GEOPHYSICAL RESEARCH LETTERS, VOL. 0, NO. 0, PAGES 0-0, M 0, 2001 On the Pacific Ocean regime shift variability of Pacific Ocean upper ocean heat content is examined for the 1948-1998 period using gridded-wide phenomenon affecting the thermal structure from 60 S to 70 N. EOF analysis of the Pacific Ocean heat content

  2. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. ???, XXXX, DOI:10.1029/, An EddyResolving Ocean Model for the Pacific1

    E-Print Network [OSTI]

    Miami, University of

    for the Pacific1 Ocean: Part 1: Deep Convection and Its Relation to2 SST Anomalies3 A. B. Kara, E. J. Metzger, H­latitudes) HYbrid Coordinate Ocean Model (HYCOM),10 configured for the Pacific Ocean (north of 20 S) is used to satellite­based products over the Pacific22 Ocean. HYCOM simulation with no assimilation of any SST gives

  3. Reconciling disparate 20th Century Indo-Pacific ocean temperature5 trends in the instrumental record6

    E-Print Network [OSTI]

    Newman, Matthew

    1 2 3 4 Reconciling disparate 20th Century Indo-Pacific ocean temperature5 trends in the Indian Ocean and western Pacific Ocean are consistent across26 the 4 datasets, it is uncertain whether theories for the response of the tropical Pacific Ocean to an1 increase in greenhouse gases. Assuming

  4. Shipboard Measurements and Estimations of AirSea Fluxes in the Western Tropical Pacific Ocean

    E-Print Network [OSTI]

    California at Irvine, University of

    Ship­board Measurements and Estimations of Air­Sea Fluxes in the Western Tropical Pacific Ocean E dur­ ing the Tropical Ocean Global Atmosphere (TOGA) Coupled Ocean and Atmospheric Response of the surface­layer turbulence properties are compared with those from previous land and ocean results. Momentum

  5. Intercomparison of Biogeochemical Properties at Atlantic and Pacific Observatory Sites Using Ocean Data and a PARADIGM Model

    E-Print Network [OSTI]

    Yoder, James S.

    Intercomparison of Biogeochemical Properties at Atlantic and Pacific Observatory Sites Using Ocean compare 34 locations in the Atlantic and Pacific Oceans with respect to key upper ocean ecological by SeaWiFS mean chlorophyll: low chlorophyll ocean gyres, comparatively high chlorophyll ocean margin

  6. Lost at Sea: Hurricane Force Wind Fields and the North Pacific Ocean Environment

    E-Print Network [OSTI]

    Businger, Steven

    Lost at Sea: Hurricane Force Wind Fields and the North Pacific Ocean Environment 1 Steven Businger and Selen Yildiz SOEST at University of Hawaii at Manoa This research is supported by ONR Lost at Sea: Hurricane Force Wind Fields and the North Pacific Ocean Environment 2 Hurricane Force (HF) Wind Fields

  7. Decadal variability of the Pacific subtropical cells and their influence on the southeast Indian Ocean

    E-Print Network [OSTI]

    Feng, Ming

    Click Here for Full Article Decadal variability of the Pacific subtropical cells records reveal that a strengthening of the Pacific subtropical cells (STCs) since the early1990's has), Decadal variability of the Pacific subtropical cells and their influence on the southeast Indian Ocean

  8. Biogeochemical and hydrographic controls on chromophoric dissolved organic matter distribution in the Pacific Ocean

    E-Print Network [OSTI]

    Siegel, David A.

    in the Pacific Ocean Chantal M. Swan a,Ã, David A. Siegel a,b , Norman B. Nelson a , Craig A. Carlson c , Elora Available online 19 September 2009 Keywords: CDOM AOU Pacific Water masses Hydrography Bio-optical a b s t r a c t Recent in situ observations of chromophoric dissolved organic material (CDOM) in the Pacific

  9. The Continental Margin is a Key Source of Iron to the HNLC North Pacific Ocean

    E-Print Network [OSTI]

    The Continental Margin is a Key Source of Iron to the HNLC North Pacific Ocean Phoebe J. Lam1 concentrations in the upper 500m of the Western Subarctic Pacific, an iron-limited High Nutrient Low Chlorophyll a key source of bioavailable Fe to the HNLC North Pacific. Keywords: iron, continental margin, HNLC 1

  10. Biophysical responses near equatorial islands in the Western Pacific Ocean during El Nio/La Nia transitions

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    Biophysical responses near equatorial islands in the Western Pacific Ocean during El Niño/La Niña 2013. [1] The biological response in the western equatorial Pacific Ocean during El Niño/La Niña responses near equatorial islands in the Western Pacific Ocean during El Niño/La Niña transitions, Geophys

  11. Proper orthogonal decomposition approach and error estimation of mixed finite element methods for the tropical Pacific Ocean

    E-Print Network [OSTI]

    Navon, Michael

    for the tropical Pacific Ocean reduced gravity model Zhendong Luo a , Jiang Zhu b , Ruiwen Wang b , I.M. Navon c Available online 8 May 2007 Abstract In this paper, the tropical Pacific Ocean reduced gravity model and the insufficient knowledge of air­sea exchange processes. The tropical Pacific Ocean reduced gravity model

  12. Large fluctuations of dissolved oxygen in the Indian and Pacific oceans during Dansgaard-Oeschger oscillations caused by variations

    E-Print Network [OSTI]

    Pedersen, Tom

    Large fluctuations of dissolved oxygen in the Indian and Pacific oceans during Dansgaard glacial Indian and Pacific oceans sediments document millennial-scale fluctuations of subsurface dissolved Hemisphere of the Indian and Pacific oceans, consistent with the paleoclimate records. Cold periods

  13. Internal variability of the tropical Pacific ocean Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts, USA

    E-Print Network [OSTI]

    Jochum, Markus

    Internal variability of the tropical Pacific ocean M. Jochum Earth, Atmospheric and Planetary model of the tropical Pacific ocean is analyzed to quantify the interannual variability caused by internal variability of ocean dynamics. It is found that along the Pacific cold tongue internal variability

  14. Subarctic Pacific evidence for a glacial deepening of the oceanic respired carbon pool S.L. Jaccard a,d,

    E-Print Network [OSTI]

    Pedersen, Tom

    Subarctic Pacific evidence for a glacial deepening of the oceanic respired carbon pool S.L. Jaccard of the overturning circulation. Volumetrically the Pacific Ocean dominates the world ocean (it is three times larger of Atmospheric and Oceanic Sciences, Princeton University, Princeton, USA c Department of Geosciences, Princeton

  15. Population structure of Manta birostris (Chondrichthyes:Mobulidae) from the Pacific and Atlantic oceans 

    E-Print Network [OSTI]

    Clark, Timothy Brian

    2002-01-01

    Sequence variation was examined in the circumtropical and highly vagile manta ray, Manta birostris, from the western and eastern Pacific oceans and the Gulf of Mexico to investigate the systematics and population structure of Manta. The entire...

  16. OligoceneMiocene tectonic evolution of the South Fiji Basin and Northland Plateau, SW Pacific Ocean: Evidence from

    E-Print Network [OSTI]

    Demouchy, Sylvie

    investigated parts of the southwest Pacific Ocean. It is a region of remnant volcanic arcs, plateaus and basins of the study area in the SW Pacific Ocean, showing geographic names and dredge locations from ChurkinOligocene­Miocene tectonic evolution of the South Fiji Basin and Northland Plateau, SW Pacific

  17. Relating spatial and temporal scales of climate and ocean variability to survival of Pacific Northwest Chinook salmon

    E-Print Network [OSTI]

    Relating spatial and temporal scales of climate and ocean variability to survival of Pacific Oregon St, Suite 200, Portland, OR 97232, U.S.A. 2 Fisheries and Oceans Canada, Pacific Biological of Washington, Seattle, WA 98195-5020, U.S.A. ABSTRACT Pacific Northwest Chinook, Oncorhynchus tshawytscha, have

  18. Striped Marlin, Tetrapturus audax, Migration Patterns and Rates in the Northeast Pacific Ocean as Determined by a Cooperative

    E-Print Network [OSTI]

    Striped Marlin, Tetrapturus audax, Migration Patterns and Rates in the Northeast Pacific Ocean, tagged and recaptured in the northeast Pacific Ocean during 1957-81 are reported by time period. Billfish tagging by marine anglers in the Pacific began in the middle 1950's when tagging equipment

  19. Central South Pacific thermocline water circulation from a high-resolution ocean model validated against satellite data

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    Central South Pacific thermocline water circulation from a high-resolution ocean model validated. Introduction [2] Most South Pacific Ocean studies have been focused on its western or eastern part, leaving 12 January 2009; accepted 28 January 2009; published 13 May 2009. [1] The oceanic circulation

  20. Impact of Tropical Cyclones on the Heat Budget of the South Pacific Ocean S. JULLIEN,* C. E. MENKES,1

    E-Print Network [OSTI]

    Impact of Tropical Cyclones on the Heat Budget of the South Pacific Ocean S. JULLIEN,* C. E. MENKES cyclones (TCs) in the South Pacific convergence zone through a complete ocean heat budget. The TC impact, in final form 4 May 2012) ABSTRACT The present study investigates the integrated ocean response to tropical

  1. Movements and behaviors of swordfish in the Atlantic and Pacific Oceans examined using pop-up satellite archival tags

    E-Print Network [OSTI]

    Hawai'i at Manoa, University of

    Movements and behaviors of swordfish in the Atlantic and Pacific Oceans examined using pop depths were signifi- cantly correlated with light penetration as measured by the diffuse attenuation words: Atlantic Ocean, deep sound scattering layer, diel migration, Pacific Ocean, satellite tags

  2. David Welch is the president of Kintama Research Services Ltd., and chief architect of the Pacific Ocean

    E-Print Network [OSTI]

    Hawai'i at Manoa, University of

    . During the next decade he was responsible for studying the ocean biology of Pacific salmon, and providedDavid Welch is the president of Kintama Research Services Ltd., and chief architect of the Pacific Ocean Shelf Tracking project (POST), which has formed the basis for the global Ocean Tracking Network

  3. Sinking fluxes of minor and trace elements in the North Pacific Ocean measured during the VERTIGO program

    E-Print Network [OSTI]

    Sinking fluxes of minor and trace elements in the North Pacific Ocean measured during the VERTIGO depths in the oceanic mesopelagic zone and at two biogeochemically contrasting sites (N. Central Pacific in the Global Ocean (VERTIGO) program, we collected and analyzed sinking particles using sediment traps at three

  4. Modal analysis of the range evolution of broadband wavefields in the North Pacific Ocean: Low mode numbers

    E-Print Network [OSTI]

    Frandsen, Jannette B.

    Modal analysis of the range evolution of broadband wavefields in the North Pacific Ocean: Low mode North Pacific Ocean are reported here. Transient wavefields in the 50­90 Hz band that were recorded numbers Ilya A. Udovydchenkova) Applied Ocean Physics and Engineering Department, Woods Hole Oceanographic

  5. East Pacific ocean eddies and their relationship to subseasonal variability in Central American wind jets

    E-Print Network [OSTI]

    Qiu, Bo

    flank of the wind jet and strengthens as it propagates offshore in the following two to three weeks Papagayo, ocean eddy formation is not well correlated with local wind jet variability. In both the GulfsEast Pacific ocean eddies and their relationship to subseasonal variability in Central American

  6. Pacific Equatorial Age Transect (PEAT): Summary As the largest ocean, the Pacific is intricately linked to major changes in the global

    E-Print Network [OSTI]

    Pacific Equatorial Age Transect (PEAT): Summary As the largest ocean, the Pacific is intricately and objectives, together with the estimated age for the oceanic crust on which the sedimentary section rests be deployed for the upper ~200 m. Table 1: Proposed Site details Penetration (m) Site-specific Objectives

  7. TSUNAMI INUNDATION MAPPING FOR OCEAN CITY, MD NGDC DEM

    E-Print Network [OSTI]

    Kirby, James T.

    TSUNAMI INUNDATION MAPPING FOR OCEAN CITY, MD NGDC DEM BY BABAK TEHRANIRAD, SAEIDEH BANIHASHEMI BY THE NATIONAL TSUNAMI HAZARD MITIGATION PROGRAM NATIONAL WEATHER SERVICE GRANT NA10NWS4670010 CENTER FOR APPLIED COASTAL RESEARCH Ocean Engineering Laboratory University of Delaware Newark, Delaware 19716 #12;Tsunami

  8. A study of lightning activity over the warm pool western Pacific Ocean (TOGA-COARE region) for 1993 

    E-Print Network [OSTI]

    Rios, Luis Alberto

    1995-01-01

    The warm pool western Pacific Ocean is an area of the equatorial tropics characterized by strong and frequent convection, and vigorous lightning activity. However, it has been noted by various researchers that the vast oceanic expanses experience...

  9. Variability of the Indo-Pacific Ocean exchanges

    E-Print Network [OSTI]

    Wunsch, Carl

    The ECCO–GODAE global estimate of the ocean circulation 1992–2007 is analyzed in the region of the Indonesian Throughflow (ITF), including the Southern Ocean flow south of Australia. General characteristics are an intense ...

  10. Temporal variability of Î? 14 C, δ 13 C, and C/N in sinking particulate organic matter at a deep time series station in the northeast Pacific Ocean

    E-Print Network [OSTI]

    Hwang, Jeomshik; Druffel, Ellen R. M; Griffin, Sheila; Smith, Kenneth L; Baldwin, Roberta J; Bauer, James E

    2004-01-01

    in the northeast Pacific Ocean, J. Geophys. Res. , 101,slope to the abyssal NE Pacific Ocean, Deep Sea Res. , Partin the eastern North Pacific Ocean, J. Geophys. Res. , 103,

  11. 232 IEEE JOURNAL OF OCEANIC ENGINEERING, VOL. 30, NO. 1, JANUARY 2005 North East Pacific Time-Integrated Undersea

    E-Print Network [OSTI]

    Frandsen, Jannette B.

    232 IEEE JOURNAL OF OCEANIC ENGINEERING, VOL. 30, NO. 1, JANUARY 2005 North East Pacific TimeGinnis, and Phil Lancaster Abstract--The objective of the North East Pacific Time-In- tegrated Undersea Networked elec- tronics, transient analysis, underwater cables. I. INTRODUCTION THE vast oceans of the world have

  12. Oceanic Control of Northeast Pacific Hurricane Activity at Interannual Timescales

    SciTech Connect (OSTI)

    Balaguru, Karthik; Leung, Lai-Yung R.; Yoon, Jin-Ho

    2013-10-16

    Despite the strong dependence of the Power Dissipation Index (PDI), which is a measure of the intensity of Tropical Cyclone (TC) activity, on tropical sea-surface temperatures (SSTs), the variations in PDI are not completely explained by SST. Here we show, using an analysis of a string of observational data sets, that the variability of the thermocline depth (TD) in the east Pacific exerts a significant degree of control on the variability of PDI in that region. On average, a deep thermocline with a larger reservoir of heat favors TC intensification by reducing SST cooling while a shallow thermocline with a smaller heat reservoir promotes enhanced SST cooling that contributes to TC decay. At interannual time scales, the variability of basin-mean TD accounts for nearly 30% of the variability in the PDI during the TC season. Also, about 20% of the interannual variability in the east Pacific basin-mean TD is due to the El Niño and the Southern Oscillation (ENSO), a dominant climate signal in this region. This study suggests that a better understanding of the factors governing the interannual variability of the TD conditions in the east Pacific and how they may change over time, may lead to an improved projection of future east Pacific TC activity.

  13. PACIFICA (PACIFic ocean Interior CArbon) Database: A Data Synthesis Resource (NDP-92, ORNL/CDIAC-159)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    Suzuki, T.; Ishii, M.; Aoyama, M. R; Christian, J. R.; Enyo, K.; Kawano, T.; Key, R. M.; Kosugi, N.; Kozyr, A.; Miller, L. A.; Murata, A.; Nakano, T.; Ono, T.; Saino, T.; Sasaki, K.; Sasano, D; Takatani, Y.; Wakita, M.; Sabine, C.

    PACIFICA (PACIFic ocean Interior CArbon) was an international collaborative project for synthesis of data on ocean interior carbon and its related parameters in the Pacific Ocean. The North Pacific Marine Science Organization (PICES), Section on Carbon and Climate (S-CC) supported the project. Hydrographic/hydrochemical datasets have been merged from a total of 272 cruises, including those from cruises conducted between the late 1980s and 2000 but not included in GLODAP, as well as CLIVAR/CO2 Repeat Hydrography datasets from the 2000s. Adjustments were calculated to account for analytical offsets in dissolved inorganic carbon, total alkalinity, salinity, oxygen, and nutrients (nitrate and nitrite, phosphate, and silicic acid) for each cruise as a result of the secondary quality control procedure, based on crossover analysis using data from deep layers (Tanhua et al., 2010). A total of 59 adjusted datasets from Line P off the west coast of Canada were also merged. Finally, the authors have produced the adjusted PACIFICA database that consists of datasets from a total of 306 cruises that also includes 34 datasets from WOCE Hydrographic Program cruises in the Pacific Ocean conducted in the 1990s. The PACIFICA database is available free of charge as a numeric data package (NDP-92) from the Carbon Dioxide Information Analysis Center (CDIAC) and the primary PACIFICA data site at pacifica.pices.jp. The NDP consists of the original cruise data files, adjusted data product, and the documentation.

  14. Data Report: Oligocene Paleoceanography of the Equatorial Pacific Ocean: Planktonic and Benthic Foraminifer Stable Isotope Results from Site 1218 

    E-Print Network [OSTI]

    Wade, Bridget, S.; P??like, Heiko

    2005-01-01

    .) Proceedings of the Ocean Drilling Program, Scientific Results Volume 199 17. DATA REPORT: OLIGOCENE PALEOCEANOGRAPHY OF THE EQUATORIAL PACIFIC OCEAN: PLANKTONIC AND BENTHIC FORAMINIFER STABLE ISOTOPE RESULTS FROM SITE 1218 1 Bridget S. Wade 2,3 and Heiko... Hemisphere. Previous work has suggested that the volume of the Antarctic ice sheet 1 Wade, B.S., and P?like, H., 2005. Data report: Oligocene paleoceanography of the equatorial Pacific Ocean: planktonic and benthic foraminifer stable isotope results from...

  15. Impact of mesoscale eddies on water transport between the Pacific Ocean and the Bering Sea

    E-Print Network [OSTI]

    Prants, S V; Budyansky, M V; Uleysky, M Yu

    2013-01-01

    Sea surface height anomalies observed by satellites in 1993--2012 are combined with simulation and observations by surface drifters and Argo floats to study water flow pattern in the Near Strait (NS) connected the Pacific Ocean with the Bering Sea. Daily Lagrangian latitudinal maps, computed with the AVISO surface velocity field, and calculation of the transport across the strait show that the flow through the NS is highly variable and controlled by mesoscale and submesoscale eddies in the area. On the seasonal scale, the flux through the western part of the NR is negatively correlated with the flux through its eastern part ($r=-0.93$). On the interannual time scale, a significant positive correlation ($r=0.72$) is diagnosed between the NS transport and the wind stress in winter. Increased southward component of the wind stress decreases the northward water transport through the strait. Positive wind stress curl over the strait area in winter--spring generates the cyclonic circulation and thereby enhances the...

  16. How ocean color can steer Pacific tropical cyclones

    E-Print Network [OSTI]

    Gnanadesikan, Anand

    Because ocean color alters the absorption of sunlight, it can produce changes in sea surface temperatures with further impacts on atmospheric circulation. These changes can project onto fields previously recognized to alter ...

  17. Mid-Cretaceous Palynoflora from Central Mid-Pacific Ocean 

    E-Print Network [OSTI]

    Hsiung, Shih-Yi

    2012-10-19

    Albian (late Early Cretaceous) pollen and spores were used to reconstruct the floral history of Allison Guyot in the Albian period, to better understand pollen and spore distributions on mid-oceanic islands, to investigate ...

  18. Ionospheric equatorial anomaly formation over Pacific and Atlantic oceans measured by NASA TOPEX satellite

    SciTech Connect (OSTI)

    Ewell, V.R.; Vladimer, J.A.; Lee, M.C. [Boston Univ., MA (United States). Electrical, Computer, and Systems Engineering Dept.; Doherty, P.H.; Decker, D.T. [Boston Coll., Newton, MA (United States). Inst. for Science Research; Anderson, D.N.; Klobuchar, J.A. [Phillips Lab., Hanscom AFB, MA (United States). Ionospheric Effects Branch

    1996-12-31

    Previous ionospheric observations have measured Total Electron Content (TEC) values at fixed land based locations. These observations suggest the existence of longitudinal variations in TEC values. Complementing ground data, the current NASA TOPEX mission is providing TEC data collected over oceans as a function of latitude, longitude and time starting from September 1992. With this broad data base, the authors show a more complete picture of the longitudinal dependence between the Atlantic and Pacific ocean regions and relate this dependence to plasma drifts. Periods during June and December solstice, and March and September equinox in the years 1992, through 1995, are picked to study the low-latitude regions spanning the Atlantic and Pacific oceans. TEC isodensity contours are presented by latitude versus longitude at common local time. They correlate these contours with results from the Phillips Laboratory ionospheric model.

  19. Low-frequency variability of the North Pacific Ocean: The roles of boundary-and wind-driven

    E-Print Network [OSTI]

    Qiu, Bo

    Low-frequency variability of the North Pacific Ocean: The roles of boundary- and wind in determining the low-frequency large-scale variability of the ocean interior through Rossby waves generated. The variability in the ocean interior is primarily driven by wind with only a minor influence from the boundary

  20. Observations and transport theory analysis of low frequency, acoustic mode propagation in the Eastern North Pacific Ocean

    E-Print Network [OSTI]

    Frandsen, Jannette B.

    in the Eastern North Pacific Ocean Tarun K. Chandrayadulaa) and John A. Colosi Naval Postgraduate School order mode statistics as a function of range and source depth are presented from the Long Range Ocean of ocean acoustics research for decades. Fluctuation statistics are crucial to achieve more coherent sig

  1. North Pacific Mesoscale Coupled Air-Ocean Simulations Compared with Observations

    SciTech Connect (OSTI)

    Koracin, Darko; Cerovecki, Ivana; Vellore, Ramesh; Mejia, John; Hatchett, Benjamin; McCord, Travis; McLean, Julie; Dorman, Clive

    2013-04-11

    Executive summary The main objective of the study was to investigate atmospheric and ocean interaction processes in the western Pacific and, in particular, effects of significant ocean heat loss in the Kuroshio and Kuroshio Extension regions on the lower and upper atmosphere. It is yet to be determined how significant are these processes are on climate scales. The understanding of these processes led us also to development of the methodology of coupling the Weather and Research Forecasting model with the Parallel Ocean Program model for western Pacific regional weather and climate simulations. We tested NCAR-developed research software Coupler 7 for coupling of the WRF and POP models and assessed its usability for regional-scale applications. We completed test simulations using the Coupler 7 framework, but implemented a standard WRF model code with options for both one- and two-way mode coupling. This type of coupling will allow us to seamlessly incorporate new WRF updates and versions in the future. We also performed a long-term WRF simulation (15 years) covering the entire North Pacific as well as high-resolution simulations of a case study which included extreme ocean heat losses in the Kuroshio and Kuroshio Extension regions. Since the extreme ocean heat loss occurs during winter cold air outbreaks (CAO), we simulated and analyzed a case study of a severe CAO event in January 2000 in detail. We found that the ocean heat loss induced by CAOs is amplified by additional advection from mesocyclones forming on the southern part of the Japan Sea. Large scale synoptic patterns with anomalously strong anticyclone over Siberia and Mongolia, deep Aleutian Low, and the Pacific subtropical ridge are a crucial setup for the CAO. It was found that the onset of the CAO is related to the breaking of atmospheric Rossby waves and vertical transport of vorticity that facilitates meridional advection. The study also indicates that intrinsic parameterization of the surface fluxes within the WRF model needs more evaluation and analysis.

  2. 137Cs(90Sr) and Pu isotopes in the Pacific Ocean sources & trends

    SciTech Connect (OSTI)

    Hamilton, T.F., Millies-Lacrox, J.C. [Service Mixte de Securite Radologique, Mondhery (France); Hong, G.H. [Korea Ocean Research and Development Institute, Ansan (Korea)

    1996-11-01

    The main source of artificial radioactivity in the world`s oceans can be attributed to worldwide fallout from atmospheric nuclear weapons testing. Measurements of selected artificial radionuclides in the Pacific Ocean were first conducted in the 1960`s where it was observed that fallout radioactivity had penetrated the deep ocean. Extensive studies carried out during the 1973-74 GEOSECS provided the first comprehensive data on the lateral and vertical distributions of {sup 9O}Sr, {sup 137}Cs and Pu isotopes in the Pacific on a basin wide scale. Estimates of radionuclide inventories in excess of amounts predicted to be delivered by global fallout alone were attributed to close-in fallout and tropospheric inputs from early U.S. tests conducted on Bikini and Enewetak Atolls in the Equatorial Pacific. In general, levels of fallout radionuclides (including {sup 9O}Sr, {sup 137}Cs and Pu isotopes) in the surface waters of the Pacific Ocean have decreased considerably over the past 4 decades and are now much more homogeneously distributed. Resuspension and the subsequent deposition of fallout radionuclides from previously deposited debris on land has become an important source term for the surface ocean. This can be clearly seen in measurements of fallout radionuclides in mineral aerosols over the Korean Peninsula (Yellow dust events). Radionuclides may also be transported from land to sea in river runoff-these transport mechanisms are more important in the Pacific Ocean where large quantities of river water and suspended sands/fluvial sediments reach the coastal zone. Another unique source of artificial radionuclides in the Pacific Ocean is derived from the slow resolubilization and transport of radionuclides deposited in contaminated lagoon and slope sediments near U.S. and French test sites. Although there is a small but significant flux of artificial radionuclides depositing on the sea floor, > 80% of the total 239, {sup 240}Pu inventory and > 95% of the total {sup 137}Cs inventory remains in the water column. Studies conducted through the 1980`s appear to be consistent with earlier findings and indicate that radionuclide inventories in mid-northern latitudes are at least a factor of two above those expected from global fallout alone. The long term persistence of close-in and/or stratospheric fallout from nuclear weapons testing in the Marshall Islands still appears to be the only plausible explanation for this anomaly.

  3. Subseasonal Variability of the Southeast Pacific Stratus Cloud Deck* International Pacific Research Center, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa,

    E-Print Network [OSTI]

    Xie, Shang-Ping

    Pacific Research Center, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa of Meteorology, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, Hawaii in the stratus cloud deck is closely related to variations in surface wind velocity, water vapor, sea level

  4. Multilateralism and International Ocean-Resources Law: Chapter 8. Ocean Policy Toward Russia & the Pacific Fisheries: The U.S. & Western Countries’ Perspective

    E-Print Network [OSTI]

    Kaczynski, Vladimir M.

    2003-01-01

    2002), Suckered at Sakhalin, The North Pacific Digest,change of the Russian ocean Sakhalin development strategies,David Gordon, Suckered at Sakhalin, T HE N ORTH P ACIFIC D

  5. Response of photosynthesis to ocean acidification

    E-Print Network [OSTI]

    Mackey, KRM; Morris, JJ; Morris, JJ; Morel, FMM; Kranz, SA

    2015-01-01

    sub- tropical North Pacific Ocean. Aquatic Microbial Ecologytropical Atlantic and Pacific Oceans and contributes sub-

  6. Computing dynamic height from temperature profiles north of 30N in the Pacific Ocean 

    E-Print Network [OSTI]

    O'Brien, Anthony

    1978-01-01

    fronts and their relation to the wind and energy flux fields. J. Geophys. Res. , 5, 557 ? 571. Sverdrup, H, U. , M. W. Johnson, and R. H. Fleming, 1942: The Oceans Their Phys7cs, Chemistry and General Biology. Prentice Hall. Stommel, H. S. , 1947... HEIGHT FROM TEMPERATURE PROFILES NORTH OP 30"N IN THE PACIFIC OCEAN A Thesis by ANTHONY O' BRIEN Submitted to the Graduate College of Texas A&M University in partial fullfillment of the requirement for the degree of 1fASTER OF SCIENCF. May 1978...

  7. Global Climate network evolves with North Atlantic Oscillation phases: Coupling to Southern Pacific Ocean

    E-Print Network [OSTI]

    Guez, Oded; Berezin, Yehiel; Wang, Yang; Havlin, Shlomo

    2013-01-01

    We construct a network from climate records of atmospheric temperature at surface level, at different geographical sites in the globe, using reanalysis data from years 1948-2010. We find that the network correlates with the North Atlantic Oscillation (NAO), both locally in the north Atlantic, and through coupling to the southern Pacific Ocean. The existence of tele-connection links between those areas and their stability over time allows us to suggest a possible physical explanation for this phenomenon.

  8. Week 4, Rain in my Brain On top of the Harbor Cone, Otago Peninsula, Pacific Ocean in the distance.

    E-Print Network [OSTI]

    Bardsley, John

    Week 4, Rain in my Brain On top of the Harbor Cone, Otago Peninsula, Pacific Ocean in the distance of the ocean or of this beautiful city from on-high and it all comes back that we're here, a dream come true

  9. Western Pacific Regional Summary Western Pacific

    E-Print Network [OSTI]

    ) of the Pacific-wide (western-central and eastern Pacific Ocean) total of Pacific bigeye tuna landings reported Fisheries Commission (WCPFC) is active in the western and central Pacific Ocean and the Inter-American Tropical Tuna Commission (IATTC) is active in the eastern Pacific Ocean. Species under the purview

  10. DECEMBER 1999 3073J O H N S O N A N D M C P H A D E N Interior Pycnocline Flow from the Subtropical to the Equatorial Pacific Ocean*

    E-Print Network [OSTI]

    Johnson, Gregory C.

    to the Equatorial Pacific Ocean* GREGORY C. JOHNSON AND MICHAEL J. MCPHADEN NOAA/Pacific Marine Environmental and Southern Hemispheres of the Pacific Ocean. In the North Pacific the pycnocline shoals and strengthens dra in the pycnocline of the central North Pacific. This study delineates this pathway and estimates an upper bound

  11. On the World-wide Circulation of the Deeper Waters of the World Ocean

    E-Print Network [OSTI]

    Reid, Joseph L

    2009-01-01

    circulation of the Pacific Ocean: Flow patterns, tracers,in preparing the figures. Fig. 1 Pacific Ocean winds Fig.2 Pacific Ocean circulation Fig. 4 Pacific Ocean potential

  12. UNIVERSITY OF NEW HAMPSHIRE CENTER OF COASTAL AND OCEAN MAPPING Camera Cage Construction

    E-Print Network [OSTI]

    New Hampshire, University of

    UNIVERSITY OF NEW HAMPSHIRE ­ CENTER OF COASTAL AND OCEAN MAPPING Camera Cage Construction Manual.......................................................................................................................................29 Camera (Electrical Components)............................................................. Error................................................................... Error! Bookmark not defined. Assemble Electrical Components

  13. Petrophysical properties of the root zone of sheeted dikes in the ocean crust: A case study from Hole ODP/IODP 1256D, Eastern Equatorial Pacific

    E-Print Network [OSTI]

    Demouchy, Sylvie

    Program) Site 1256 is located on the Cocos Plate in the Eastern Equatorial Pacific Ocean, in a 15 Ma oldPetrophysical properties of the root zone of sheeted dikes in the ocean crust: A case study from Hole ODP/IODP 1256D, Eastern Equatorial Pacific Marie Violay , Philippe A. Pezard, Benoît Ildefonse

  14. Using Satellite Ocean Color Data to Derive an Empirical Model for the Penetration Depth of Solar Radiation (Hp) in the Tropical Pacific Ocean

    E-Print Network [OSTI]

    Chen, .Dake

    the climate through the penetration depth of solar radiation in the upper ocean (Hp), a primary parameter on penetrative solar radiation in the tropical Pacific, demonstrating the dynamical implication of remotely in which incident solar radiation is absorbed in the mixed layer and the verti- cal penetration down

  15. ALIEN MAPS OF AN OCEAN-BEARING WORLD

    SciTech Connect (OSTI)

    Cowan, Nicolas B.; Agol, Eric; Meadows, Victoria S.; Robinson, Tyler [Astronomy Department and Astrobiology Program, University of Washington, Box 351580, Seattle, WA 98195 (United States); Livengood, Timothy A.; Deming, Drake [NASA Goddard Space Flight Center, Greenbelt, MD 20771 (United States); Lisse, Carey M. [Johns Hopkins University Applied Physics Laboratory, SD/SRE, MP3-E167, 11100 Johns Hopkins Road, Laurel, MD 20723 (United States); A'Hearn, Michael F.; Wellnitz, Dennis D. [Department of Astronomy, University of Maryland, College Park, MD 20742 (United States); Seager, Sara [Department of Earth, Atmospheric, and Planetary Sciences, Department of Physics, Massachusetts Institute of Technology, 77 Massachusetts Ave. 54-1626, MA 02139 (United States); Charbonneau, David [Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138 (United States)], E-mail: cowan@astro.washington.edu

    2009-08-01

    When Earth-mass extrasolar planets first become detectable, one challenge will be to determine which of these worlds harbor liquid water, a widely used criterion for habitability. Some of the first observations of these planets will consist of disc-averaged, time-resolved broadband photometry. To simulate such data, the Deep Impact spacecraft obtained light curves of Earth at seven wavebands spanning 300-1000 nm as part of the EPOXI mission of opportunity. In this paper, we analyze disc-integrated light curves, treating Earth as if it were an exoplanet, to determine if we can detect the presence of oceans and continents. We present two observations each spanning 1 day, taken at gibbous phases of 57 deg. and 77 deg., respectively. As expected, the time-averaged spectrum of Earth is blue at short wavelengths due to Rayleigh scattering, and gray redward of 600 nm due to reflective clouds. The rotation of the planet leads to diurnal albedo variations of 15%-30%, with the largest relative changes occurring at the reddest wavelengths. To characterize these variations in an unbiased manner, we carry out a principal component analysis of the multi-band light curves; this analysis reveals that 98% of the diurnal color changes of Earth are due to only two dominant eigencolors. We use the time variations of these two eigencolors to construct longitudinal maps of the Earth, treating it as a non-uniform Lambert sphere. We find that the spectral and spatial distributions of the eigencolors correspond to cloud-free continents and oceans despite the fact that our observations were taken on days with typical cloud cover. We also find that the near-infrared wavebands are particularly useful in distinguishing between land and water. Based on this experiment, we conclude that it should be possible to infer the existence of water oceans on exoplanets with time-resolved broadband observations taken by a large space-based coronagraphic telescope.

  16. Center for Coastal & Ocean Mapping NOAA-UNH Joint Hydrographic Center

    E-Print Network [OSTI]

    New Hampshire, University of

    - age has been incorporated into standard software for offshore mapping and, as it continues to be refined, will be a boon not only for habitat mapping but ocean engineering projects--aquaculture, wind farms, deep-ocean struc- tures--that require highly accurate seafloor characterization. Seafloor

  17. Western Pacific Regional Summary Western Pacific

    E-Print Network [OSTI]

    -central and eastern Pacific Ocean) total of Pacific bigeye tuna landings reported in 2007. Currently (WCPFC) is active in the western and central Pacific Ocean and the Inter-American Tropical Tuna Commission (IATTC) is active in the eastern Pacific Ocean. Species under the purview of the WCPFC and IATTC

  18. Western Pacific Regional Summary Western Pacific

    E-Print Network [OSTI]

    Pacific Ocean) total of Pacific bigeye tuna landings reported in 2007. Currently, there are no catch share in the western and central Pacific Ocean and the Inter-American Tropical Tuna Commission (IATTC) is active in the eastern Pacific Ocean. Species under the purview of the WCPFC and IATTC migrate across international

  19. Plastic particles in coastal pelagic ecosystems of the Northeast Pacific ocean Miriam J. Doyle a,*, William Watson b

    E-Print Network [OSTI]

    Plastic particles in coastal pelagic ecosystems of the Northeast Pacific ocean Miriam J. Doyle a 2010 Accepted 11 October 2010 Keywords: Plastic particles Fragments Fibers Pellets Pelagic ecosystems the distribution, abundance and characteristics of plastic particles in plankton samples collected routinely

  20. and new production rates from several locations in the coastal and open Pacific Ocean. They also demonstrated

    E-Print Network [OSTI]

    Buesseler, Ken

    and new production rates from several locations in the coastal and open Pacific Ocean. They also approximated the large-scale rate of new production. In 1967, Richard Dugdale and John Goering had defined new production as the fraction of the overall net primary production that was supported by external, or "new

  1. Tidal constituent database. West Coast of the United States and Eastern North pacific ocean. Technical note

    SciTech Connect (OSTI)

    NONE

    1995-01-01

    This technical note describes a database of tidal elevation boundary condition information generated in support of the `Long-Term Fate of Dredged Material Disposed in Open Water` research of the Dredging Research Program (DRP), being conducted at the U.S. Army Engineer Waterways Experiment Station. The database, described in detail by Hench and others (1994), allows the user to manually generate time series of tidal elevations or to use a program to access the full database to generate time series of both tidal elevations and currents for any location along the West Coast of the United States and Eastern North Pacific Ocean, extending from Seal Cape on Unimak Island, Alaska, in the North to Punta Parada, Peru, in the South. The land boundary includes the Pacific shorelines of Alaska, Canada, mainland United States, Mexico, Guatemala, El Salvador, Nicaragua, Costa Rica, Panama, Columbia, and Northern Peru. Although the capability to generate these time series was developed to provide input to the Long-Term Fate and Stability Model (LTFATE), the generated time series can be used for any application requiring tidal forcing data.

  2. 5.12 Ocean-Derived Aerosol and Its Climate Impacts PK Quinn and TS Bates, NOAA Pacific Marine Environmental Laboratory, Seattle, WA, USA

    E-Print Network [OSTI]

    5.12 Ocean-Derived Aerosol and Its Climate Impacts PK Quinn and TS Bates, NOAA Pacific Marine Environmental Laboratory, Seattle, WA, USA Published by Elsevier Ltd. 5.12.1 Introduction 317 5.12.2 Ocean-Derived Aerosol Production Mechanisms 317 5.12.3 Radiative Effects of Ocean-Derived Aerosol 319 5.12.3.1 Aerosol

  3. Photoproduction of carbonyl sulfide in south Pacific Ocean waters as a function of irradiation wavelength

    SciTech Connect (OSTI)

    Weiss, P.S. [Univ. of Washington, Seattle, WA (United States)] [Univ. of Washington, Seattle, WA (United States); [Pacific Marine Environmental Lab., Seattle, WA (United States); Johnson, J.E. [Pacific Marine Environmental Lab., Seattle, WA (United States)] [Pacific Marine Environmental Lab., Seattle, WA (United States); [Univ. of Washington, Seattle, WA (United States); Andrews, S.S.; Zafiriou, O.C. [Woods Hole Oceanographic Institute, MA (United States)] [Woods Hole Oceanographic Institute, MA (United States)

    1995-02-01

    Carbonyl sulfide (OCS) photoproduction rates were measured at selected wavelengths of ultraviolet light between 297 and 405 nm in sea water samples from the southern Pacific Ocean. Near-surface and column production rate spectra for natural sunlit waters were calculated using sea-surface sunlight data measured near the austral summer solstice. These plots show that photoproduction rates are at a maximum at 313 nm in tropical waters and at 336 nm in Antarctic waters. Tropical surface and column rates were found to be 68 pM/day and 360 nmol/m{sup 2}/day, respectively, and Antarctic surface and column rates were found to be 101 pM/day and 620 nmol/m{sup 2}/day, respectively. A high degree of variability was observed between photoproduction rates from different ocean regions, with coastal rates being the highest, suggesting that natural environmental variability is an important factor. Photoproduction rates at 297 nm were found to be constant at individual locations with increasing irradiation time. Relative photoproduction rates from this work are compared to previously measured rates from coastal sea water. 19 refs., 4 figs., 1 tab.

  4. Alien Maps of an Ocean-Bearing World

    E-Print Network [OSTI]

    Cowan, N B; Meadows, V S; Robinson, T; Livengood, T A; Deming, D; Lisse, C M; A'Hearn, M F; Wellnitz, D D; Seager, S; Charbonneau, D

    2009-01-01

    [Abridged] To simulate the kinds of observations that will eventually be obtained for exoplanets, the Deep Impact spacecraft obtained light curves of Earth at seven wavebands spanning 300-1000 nm as part of the EPOXI mission of opportunity. In this paper we analyze disc-integrated light curves, treating Earth as if it were an exoplanet, to determine if we can detect the presence of oceans and continents. We present two observations each spanning one day, taken at gibbous phases. The rotation of the planet leads to diurnal albedo variations of 15-30%, with the largest relative changes occuring at the reddest wavelengths. To characterize these variations in an unbiased manner we carry out a principal component analysis of the multi-band light curves; this analysis reveals that 98% of the diurnal color changes of Earth are due to only 2 dominant eigencolors. We use the time-variations of these two eigencolors to construct longitudinal maps of the Earth, treating it as a non-uniform Lambert sphere. We find that t...

  5. Impacts of ocean acidification and mitigative hydrated lime addition on Pacific oyster larvae

    E-Print Network [OSTI]

    aquaculture; Pacific Northwest #12;v Dedication Tomymother,Ann.Throughlifeyouhaveshownmewhat realstrengthis.......................................................................................................................... iv Dedication...............

  6. Physical Mechanisms for the Maintenance of GCM-Simulated Madden-Julian Oscillation over the Indian Ocean and Pacific

    SciTech Connect (OSTI)

    Deng, Liping; Wu, Xiaoqing

    2011-05-05

    The kinetic energy budget is conducted to analyze the physical processes responsible for the improved Madden-Julian Oscillation (MJO) simulated by the Iowa State University general circulation models (ISUGCM). The modified deep convection scheme that includes the revised convection closure, convection trigger condition and convective momentum transport (CMT) enhances the equatorial (10oS-10oN) MJO-related perturbation kinetic energy (PKE) in the upper troposphere and leads to more robust and coherent eastward propagating MJO signal. In the MJO source region-the Indian Ocean (45oE-120oE), the upper-tropospheric MJO PKE is maintained by the vertical convergence of wave energy flux and the barotropic conversion through the horizontal shear of mean flow. In the convectively active region-the western Pacific (120oE-180o), the upper-tropospheric MJO PKE is supported by the convergence of horizontal and vertical wave energy fluxes. Over the central-eastern Pacific (180o-120oW), where convection is suppressed, the upper-tropospheric MJO PKE is mainly due to the horizontal convergence of wave energy flux. The deep convection trigger condition produces stronger convective heating which enhances the perturbation available potential energy (PAPE) production and the upward wave energy fluxes, and leads to the increased MJO PKE over the Indian Ocean and western Pacific. The trigger condition also enhances the MJO PKE over the central-eastern Pacific through the increased convergence of meridional wave energy flux from the subtropical latitudes of both hemispheres. The revised convection closure affects the response of mean zonal wind shear to the convective heating over the Indian Ocean and leads to the enhanced upper-tropospheric MJO PKE through the barotropic conversion. The stronger eastward wave energy flux due to the increase of convective heating over the Indian Ocean and western Pacific by the revised closure is favorable to the eastward propagation of MJO and the convergence of horizontal wave energy flux over the central-eastern Pacific. The convection-induced momentum tendency tends to decelerate the upper-tropospheric wind which results in a negative work to the PKE budget in the upper troposphere. However, the convection momentum tendency accelerates the westerly wind below 800 hPa over the western Pacific, which is partially responsible for the improved MJO simulation.

  7. ENSO regimes and the late 1970's climate shift: The role of synoptic weather and South Pacific ocean spiciness

    SciTech Connect (OSTI)

    O'Kane, Terence J.; Matear, Richard J.; Chamberlain, Matthew A.; Oke, Peter R.

    2014-08-15

    South Pacific subtropical density compensated temperature and salinity (spiciness) anomalies are known to be associated with decadal equatorial variability, however, the mechanisms by which such disturbances are generated, advect and the degree to which they modulate the equatorial thermocline remains controversial. During the late 1970's a climate regime transition preceded a period of strong and sustained El Nino events. Using an ocean general circulation model forced by the constituent mechanical and thermodynamic components of the reanalysed atmosphere we show that the late 1970's transition coincided with the arrival of a large-scale, subsurface cold and fresh water anomaly in the central tropical Pacific. An ocean reanalysis for the period 1990–2007 that assimilates subsurface Argo, XBT and CTD data, reveals that disturbances occur due to the subduction of negative surface salinity anomalies from near 30° S, 100° W which are advected along the ?=25–26 kgm{sup ?3} isopycnal surfaces. These anomalies take, on average, seven years to reach the central equatorial Pacific where they may substantially perturb the thermocline before the remnants ultimately ventilate in the region of the western Pacific warm pool. Positive (warm–salty) disturbances, known to occur due to late winter diapycnal mixing and isopycnal outcropping, arise due to both subduction of subtropical mode waters and subsurface injection. On reaching the equatorial band (10° S–0° S) these disturbances tend to deepen the thermocline reducing the model's ENSO. In contrast the emergence of negative (cold–fresh) disturbances at the equator are associated with a shoaling of the thermocline and El Nino events. Process studies are used to show that the generation and advection of anomalous density compensated thermocline disturbances critically depend on stochastic forcing of the intrinsic ocean by weather. We further show that in the absence of the inter-annual component of the atmosphere forcing Central Pacific El Nino events are manifest.

  8. Character of the diatom assemblage spanning a depositional transition in the Eastern Equatorial Pacific Ocean at 6.6 Ma 

    E-Print Network [OSTI]

    Brookshire, Brian Neville, Jr.

    2005-02-17

    in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2003 Major Subject: Oceanography CHARACTER OF THE DIATOM ASSEMBLAGE SPANNING A DEPOSITIONAL TRANSITION IN THE EASTERN EQUATORIAL PACIFIC OCEAN AT 6.6 Ma A Thesis... by BRIAN NEVILLE BROOKSHIRE JR. Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Approved as to style and content by...

  9. PACIFIC COAST SALMON pacific Coast Salmon

    E-Print Network [OSTI]

    and central North Pacific Ocean. These species are only vulnerable to shore-based Photo above: Male coho in the Pacific Ocean, Puget Sound, and in freshwater rivers on their spawning migrations. All recreational. In the Pacific Ocean all harvest is by trolling; in Puget Sound, gillnets and purse seines are used in addition

  10. North Pacific carbon cycle response to climate variability on seasonal to decadal timescales

    E-Print Network [OSTI]

    2006-01-01

    in the subarctic North Pacific Ocean, Global Biogeochem.of the tropical Pacific Ocean: I. Seasonal and interannualthe subtropical North Pacific Ocean, Nature, 424, 754 – 757.

  11. Strengthening of the Pacific Equatorial Undercurrent in the SODA Reanalysis: Mechanisms, Ocean Dynamics, and Implications

    E-Print Network [OSTI]

    Karnauskas, Kristopher B.

    Several recent studies utilizing global climate models predict that the Pacific Equatorial Undercurrent (EUC) will strengthen over the twenty-first century. Here, historical changes in the tropical Pacific are investigated ...

  12. Ship Observations of the Tropical Pacific Ocean along the Coast of South America S. P. DE SZOEKE, C. W. FAIRALL, AND SERGIO PEZOA

    E-Print Network [OSTI]

    Kurapov, Alexander

    of upwelling, surface fluxes, and transport, which in turn depend on the wind and solar forcing at the ocean surface. Southeasterly winds blow parallel to the coast in the Southern Hemisphere, causing offshore EkmanShip Observations of the Tropical Pacific Ocean along the Coast of South America S. P. DE SZOEKE, C

  13. INTERNATIONAL PACIFIC RESEARCH CENTER

    E-Print Network [OSTI]

    Wang, Yuqing

    environmental change and Asia-Pacific climate. The Asia-Pacific Data-Research Center (APDRC): To provide-Australian Monsoon System 14 Impacts of Global Environmental Change 21 Asia-Pacific Data-Research Center 27 Center 1 The Year's Highlights 3 Indo-Pacific Ocean Climate 4 Regional-Ocean Influences 10 Asian

  14. INTERNATIONAL PACIFIC RESEARCH CENTER

    E-Print Network [OSTI]

    Wang, Yuqing

    environmental change and Asia-Pacific climate. The Asia-Pacific Data-Research Center (APDRC): To provide Research Center 1 2 The Year's Highlights 3 Research Accomplishments Indo-Pacific Ocean Climate 4 Regional-Ocean Influences 15 Asian-Australian Monsoon System 19 Impacts of Global Environmental Change 29 Asia-Pacific Data

  15. International Pacific Research Center

    E-Print Network [OSTI]

    Wang, Yuqing

    environmental change and Asia-Pacific climate. The Asia-Pacific Data-Research Center (APDRC): To provide-Australian Monsoon System 19 Impacts of Global Environmental Change 36 Asia-Pacific Data-Research Center 45 Center i Foreword ii iv Indo-Pacific Ocean Climate 1 Regional-Ocean Influences 13 Asian

  16. Regional Summary Western Pacific Management Context

    E-Print Network [OSTI]

    .5 million pounds) of the Pacific-wide (western-central and eastern Pacific Ocean) total of Pacific bigeye Ocean and the Inter-American Tropical Tuna Commission (IATTC) is active in the eastern Pacific Ocean coordinated management between countries with fishing interests in the Pacific Ocean. The annual bigeye tuna

  17. Methane oxidation in the eastern tropical North Pacific Ocean water column

    E-Print Network [OSTI]

    2015-01-01

    PACK ET AL. EASTERN PACIFIC METHANE OXIDATIONA method for measuring methane oxidation rates using low-levels of C-labeled methane and accelerator mass

  18. The Golden Gate Textile Barrier: Preserving California Bay of San Francisco from a Rising North Pacific Ocean

    E-Print Network [OSTI]

    Richart B. Cathcart; Alexander A. Bolonkin

    2007-02-04

    Climate change in California may require construction of a barrier separating the Pacific Ocean from San Francisco Bay and the Sacramento River-San Joaquin River Delta simply because Southern California is remarkably dependent on freshwater exported from the Delta. We offer a new kind of salt barrier, a macroproject built of impermeable textile materials stretched across the Golden Gate beneath the famous bridge. We anticipate it might eventually substitute for a recently proposed San Francisco In-Stream Tidal Power Plant harnessing a 1.7 m tide at the Bay entrance if future climate conditions Statewide is conducive. First-glance physics underpin our macroproject.

  19. The Golden Gate Textile Barrier: Preserving California Bay of San Francisco from a Rising North Pacific Ocean

    E-Print Network [OSTI]

    Cathcart, R B; Bolonkin, Alexander A.; Cathcart, Richart B.

    2007-01-01

    Climate change in California may require construction of a barrier separating the Pacific Ocean from San Francisco Bay and the Sacramento River-San Joaquin River Delta simply because Southern California is remarkably dependent on freshwater exported from the Delta. We offer a new kind of salt barrier, a macroproject built of impermeable textile materials stretched across the Golden Gate beneath the famous bridge. We anticipate it might eventually substitute for a recently proposed San Francisco In-Stream Tidal Power Plant harnessing a 1.7 m tide at the Bay entrance if future climate conditions Statewide is conducive. First-glance physics underpin our macroproject.

  20. A model of the ocean migration of Pacific salmon Chloe Bracis

    E-Print Network [OSTI]

    Washington at Seattle, University of

    advection by ocean currents with fish swimming behavior to model trajectories of salmon. The behavior rules are based on possible responses to components of the earth's magnetic field, and the ocean currents the high seas to the Columbia River, including the effects of interannual variability in ocean currents

  1. A Spatial Deconvolution of Molecular Signals in Oceanic Dissolved Organic Matter

    E-Print Network [OSTI]

    Meador, Travis B

    2008-01-01

    subtropical North Pacific Ocean. Limnol. Oceanogr. 47: 1595-the subtropical North Pacific Ocean. Nature 388: Karl, D. ,central equatorial Pacific Ocean, 1992: Daily and finescale

  2. A spatial deconvolution of molecular signals in oceanic dissolved organic matter

    E-Print Network [OSTI]

    Meador, Travis Blake

    2008-01-01

    subtropical North Pacific Ocean. Limnol. Oceanogr. 47: 1595-the subtropical North Pacific Ocean. Nature 388: Karl, D. ,in the subtropical North Pacific Ocean. Nature 388: Karl, D;

  3. Module for the Ocean Environment Prepared for the NOAA Fisheries, Northwest Regional Office

    E-Print Network [OSTI]

    ................................................................................................ 11 3.4 North Pacific Ocean ............................................................................................................................ 19 4.1.3. North Pacific Ocean ............................................................................................................................ 25 4.2.3. North Pacific Ocean

  4. Passive microwave observations of mesoscale convective systems over the tropical Pacific Ocean 

    E-Print Network [OSTI]

    McGaughey, Gary Rae

    1994-01-01

    the Advanced Microwave Precipitation Radiometer (AMPR) aboard the NASA ER2 during the Tropical Ocean and Global Atmosphere Coupled-Ocean Atmosphere Response Experiment (TOGA-COARE). The AMPR measures linearly polarized radiation at 10.7, 19.35, 37. 1, and 85...

  5. Comparison of the Carbon System Parameters at the Global CO2 Survey Crossover Locations in the North and South Pacific Ocean, 1990-1996

    SciTech Connect (OSTI)

    Feely, Richard A [NOAA, Pacific Marine Environmental Laboratory (PMEL); Lamb, Marilyn F. [NOAA, Pacific Marine Environmental Laboratory (PMEL); Greeley, Dana J. [NOAA, Pacific Marine Environmental Laboratory (PMEL); Wanninkhof, Rik [NOAA, Atlantic Oceanographic and Meteorological Laboratory (AOML)

    1999-10-01

    As a collaborative program to measure global ocean carbon inventories and provide estimates of the anthropogenic carbon dioxide (C02) uptake by the oceans. the National Oceanic and Atmospheric Administration and the U.S. Department of Energy have sponsored the collection of ocean carbon measurements as part of the World Ocean Circulation Experiment and Ocean-Atmosphere Carbon Exchange Study cruises. The cruises discussed here occurred in the North and South Pacific from 1990 through 1996. The carbon parameters from these 30 crossover locations have been compared to ensure that a consistent global data set emerges from the survey cruises. !'he results indicate that for dissolved inorganic carbon. fugacity of C02• and pH. the a~:,rreements at most crossover locations are well within the design specifications for the global CO) survey: whereas. in the case of total alkaliniry. the agreement between crossover locations is not as close.

  6. A Review of the Systematics of Angel Sharks Emphasizing the Species of the Eastern Pacific Region with a Modified Set of Morphometrics for Order Squatiniformes

    E-Print Network [OSTI]

    Alioto, Dominic

    2012-01-01

    occurring in the eastern Pacific Ocean. Ayers compared hisoccurring in the eastern Pacific Ocean. It remains possibleof the Atlantic and Pacific Oceans. Squatiniformes are very

  7. Talley, L.D. 2013. Closure of the global overturning circulation through the Indian, Pacific, and Southern Oceans: Schematics and transports. Oceanography 26(1):8097,

    E-Print Network [OSTI]

    Talley, Lynne D.

    , Pacific, and Southern Oceans: Schematics and transports. Oceanography 26(1):80­97, http://dx.doi.org/10 in Oceanography, Volume 26, Number 1, a quarterly journal of e Oceanography Society. Copyright 2013 by e Oceanography Society. All rights reserved. USAGE Permission is granted to copy this article for use in teaching

  8. Methane oxidation in the eastern tropical North Pacific Ocean water column

    E-Print Network [OSTI]

    2015-01-01

    of methane in distilled water and seawater, J. Chem. Eng.Paci?c (ETP) Ocean • Water column MO x strongly mitigatesD. M. Lavoie (1983), Upper water column methane geochemistry

  9. Causes of Ocean Surface temperature Changes in Atlantic and Pacific Topical Cyclogenesis Regions

    E-Print Network [OSTI]

    2006-01-01

    Causes of Ocean Surface Temperature Changes in Atlantic andt in understanding the causes of such changes. B. D. Santerto study the possible causes of SST changes in Atlantic and

  10. Tropical Ocean Climate Study (TOCS) and Japan-United States Tropical Ocean Study (JUSTOS) on the R/V KAIYO, 25 Jan to 2 March 1997, to the Tropical Western Pacific Ocean BNL component

    SciTech Connect (OSTI)

    Reynolds, R.M.; Smith, S.

    1997-04-11

    The Japanese U.S. Tropical Ocean Study (JUSTOS) cruise on the R/V KAIYO in the Tropical Western Pacific Ocean was a collaborative effort with participants from the Japanese Marine Science and Technology Center (JAMSTEC), the National Center for Atmospheric Research (NCAR), and Brookhaven National Laboratory BNL. This report is a summary of the instruments, measurements, and initial analysis of the BNL portion of the cruise only. It includes a brief description of the instrument system, calibration procedures, problems and resolutions, data collection, processing and data file descriptions. This is a working document, which is meant to provide both a good description of the work and as much information as possible in one place for future analysis.

  11. PACIFIC HIGHLY MIGR ATORY PEL AGIC FISHERIES pacific highly migratory

    E-Print Network [OSTI]

    the Pacific Ocean, from the tropics to temperate latitudes. Many of these fishes routinely travel great highly migratory species throughout the Pacific Ocean. Some of the fleets are capable of operating across the Pacific as well as in other oceans during a single fishing season. These fleets use larger purse

  12. Variation of surface currents and effects on dispersion in the Tropical Pacific Ocean 

    E-Print Network [OSTI]

    Horne, Doyle Jackson

    1980-01-01

    annual scale, the ITCZ is very well defined east of 170 'W and o occurs at around 8 N. West of 170 the light variable winds 0 o of the doldrums separate the two systems. The position of the ITCZ varies seasonally following the sun toward the summer... (Tabata, 197 5) North Ecuatorial Countercurrent The North Ecuatorial Countercurrent flows eastward against the wind between 4'N laf. and 10'N lat. across the entire Pacific transporting warm water from west to east. The flow is in approximate...

  13. Causes of Ocean Surface temperature Changes in Atlantic andPacific Topical Cyclogenesis Regions

    SciTech Connect (OSTI)

    Santer, B.D.; Wigley, T.M.L.; Gleckler, P.J.; Bonfils, C.; Wehner, M.F.; AchutaRao, K.; Barnett, T.P.; Boyle, J.S.; Bruggemann, W.; Fiorino, M.; Gillett, N.; Hansen, J.E.; Jones, P.D.; Klein, S.A.; Meehl,G.A.; Raper, S.C.B.; Reynolds, R.W.; Stott, P.A.; Taylor, K.E.; Washington, W.M.

    2006-01-31

    Previous research has identified links between changes in sea surface temperature (SST) and hurricane intensity. We use climate models to study the possible causes of SST changes in Atlantic and Pacific tropical cyclogenesis regions. The observed SST increases in these regions range from 0.32 to 0.67 C over the 20th century. The 22 climate models examined here suggest that century-timescale SST changes of this magnitude cannot be explained solely by unforced variability of the climate system, even under conservative assumptions regarding the magnitude of this variability. Model simulations that include external forcing by combined anthropogenic and natural factors are generally capable of replicating observed SST changes in both tropical cyclogenesis regions.

  14. Comparison of reduced-order, sequential and variational data assimilation methods in the tropical Pacific Ocean

    E-Print Network [OSTI]

    Robert, Céline; Verron, Jacques

    2006-01-01

    This paper presents a comparison of two reduced-order, sequential and variational data assimilation methods: the SEEK filter and the R-4D-Var. A hybridization of the two, combining the variational framework and the sequential evolution of covariance matrices, is also preliminarily investigated and assessed in the same experimental conditions. The comparison is performed using the twin-experiment approach on a model of the Tropical Pacific domain. The assimilated data are simulated temperature profiles at the locations of the TAO/TRITON array moorings. It is shown that, in a quasi-linear regime, both methods produce similarly good results. However the hybrid approach provides slightly better results and thus appears as potentially fruitful. In a more non-linear regime, when Tropical Instability Waves develop, the global nature of the variational approach helps control model dynamics better than the sequential approach of the SEEK filter. This aspect is probably enhanced by the context of the experiments in tha...

  15. Regional Summary Western Pacific Management Context

    E-Print Network [OSTI]

    -central and eastern Pacific Ocean) total of Pacific bigeye tuna landings reported in 2009. Currently (WCPFC) is active in the western and central Pacific Ocean and the Inter-American Tropical Tuna Commission (IATTC) is active in the eastern Pacific Ocean. Species under the purview of the WCPFC and IATTC

  16. NE Pacific St. NE Pacific St.

    E-Print Network [OSTI]

    Lake W ashington Ship Canal NE Pacific St. NE Pacific St. NE Boat St. 15th Ave NE 15thAveNE UniversityWayNE BrooklynAveNE NE Pacific St. MontlakeBlvdNE MontlakeBlvdNE Pacific Place NE University Burke-Gilman Trail METRO NW A CD D EF F GHI H J RR BB CC EE AA Rotunda Cafe Ocean Sciences Hitchcock

  17. UH Parking Access & Mid-Pacific Institute

    E-Print Network [OSTI]

    Pacific Ocean Science & Technology Kuykendall Annex Information Technology Center Krauss Hall Holmes HallStairs Pond UH Parking Access & Mid-Pacific Institute Exit Dole Street Offices Multipurpose

  18. Surface and free tropospheric sources of methanesulfonic acid over the tropical Pacific Ocean

    SciTech Connect (OSTI)

    Zhang, Yuzhong; Wang, Yuhang; Gray, Burton A.; Gu, Dasa; Mauldin, L.; Cantrell, Chris; Bandy, Alan R.

    2014-07-28

    The production of sulfate aerosols through marine sulfur chemistry is critical to the climate system. However, not all sulfur compounds have been studied in detail. One such compound is methanesulfonic acid (MSA). In this study, we use a one-dimensional chemical transport model to analyze observed vertical profiles of gas-phase MSA during the Pacific Atmospheric Sulfur Experiment (PASE). The observed sharp decrease in MSA from the surface to 600m implies a surface source of 4.0×107 molecules/cm2/s. Evidence suggests that this source is photolytically enhanced. We also find that the observed large increase of MSA from the boundary layer into the lower free troposphere (1000-2000m) results mainly from the degassing of MSA from dehydrated aerosols. We estimate a source of 1.2×107 molecules/cm2/s through this pathway. This source of soluble MSA potentially provides an important precursor for new particle formation in the free troposphere over tropics, affecting the climate system through aerosol-cloud interactions.

  19. Part IV: Other International Arrangement of Interest Asia Pacific Economic Cooperation (APEC) Oceans and Fisheries Working Group

    E-Print Network [OSTI]

    and economic cooperation among economies around the Pacific Rim. APEC members account for over 90% of globalPart IV: Other International Arrangement of Interest 166 Asia Pacific Economic Cooperation (APEC

  20. The Acoustic Thermometry of Ocean Climate (ATOC) Project: Towards depth-averaged temperature maps of the North Pacific Ocean

    E-Print Network [OSTI]

    Dushaw, Brian

    Seamount off the coast of California, the other located north of Kauai, Hawaii. Transmissions from of acoustic travel times from the Pioneer Seamount and Kauai transmissions are about 1 1/2 and 1 year long Seamount near San Francisco in October 1995 and on the north slope of the Hawaiian island of Kauai in July

  1. Biological and physical regulation of the oceanic fixed nitrogen reservoir

    E-Print Network [OSTI]

    Weber, Thomas Smith

    2013-01-01

    2 in the subtropical North Pacific Ocean. Nature 412: 635-38in the eastern tropical Pacific Ocean. Marine Chemistry 16:and N 2 fixation in the Pacific Ocean. Global Biogeochemical

  2. flow beneath the East Pacific Rise. Nature 402, 282285 (1999). 14. Grove, T. L., Kinzler, R. J. & Bryan, W. B. in Mantle Flow and Melt Generation at Mid-Ocean Ridges (eds

    E-Print Network [OSTI]

    1999-01-01

    flow beneath the East Pacific Rise. Nature 402, 282­285 (1999). 14. Grove, T. L., Kinzler, R. J. & Bryan, W. B. in Mantle Flow and Melt Generation at Mid-Ocean Ridges (eds Morgan, J. P., Blackman, D. K. Dick, H. J. B. in Magmatism in the Ocean Basins (eds Sounders, A. D. & Norry, M. J.) 71­105 (Geol. Soc

  3. Comparison of Moist Static Energy and Budget between the GCM-Simulated Madden–Julian Oscillation and Observations over the Indian Ocean and Western Pacific

    SciTech Connect (OSTI)

    Wu, Xiaoqing; Deng, Liping

    2013-07-01

    The moist static energy (MSE) anomalies and MSE budget associated with the Madden–Julian oscillation (MJO) simulated in the Iowa State University General Circulation Model (ISUGCM) over the Indian and Pacific Oceans are compared with observations. Different phase relationships between MJO 850-hPa zonal wind, precipitation, and surface latent heat flux are simulated over the Indian Ocean and western Pacific, which are greatly influenced by the convection closure, trigger conditions, and convective momentum transport (CMT). The moist static energy builds up from the lower troposphere 15–20 days before the peak of MJO precipitation, and reaches the maximum in the middle troposphere (500–600 hPa) near the peak of MJO precipitation. The gradual lower-tropospheric heating and moistening and the upward transport of moist static energy are important aspects of MJO events, which are documented in observational studies but poorly simulated in most GCMs. The trigger conditions for deep convection, obtained from the year-long cloud resolving model (CRM) simulations, contribute to the striking difference between ISUGCM simulations with the original and modified convection schemes and play the major role in the improved MJO simulation in ISUGCM. Additionally, the budget analysis with the ISUGCM simulations shows the increase in MJO MSE is in phase with the horizontal advection of MSE over the western Pacific, while out of phase with the horizontal advection of MSE over the Indian Ocean. However, the NCEP analysis shows that the tendency of MJO MSE is in phase with the horizontal advection of MSE over both oceans.

  4. Abundance and ecological implications of microplastic debris in the North Pacific Subtropical Gyre

    E-Print Network [OSTI]

    Goldstein, Miriam Chanita

    2012-01-01

    of the central North Pacific ocean. Nature 241:271–271. doi:waste distributions in Pacific Ocean. Nature 247:30–32. doi:of the central North Pacific ocean. Nature 241:271–271. doi:

  5. Mechanisms controlling dissolved iron distribution in the North Pacific: A model study

    E-Print Network [OSTI]

    2011-01-01

    latitude sites in the Pacific?Ocean, J. Geophys. Res. , 96 (of the equatorial Pacific Ocean, Nature, 371(6493), 123–129,and western North Pacific Ocean, Geophys. Res. Lett. , 33,

  6. Diurnal cycle of the Intertropical Convergence Zone in the east Pacific

    E-Print Network [OSTI]

    Bain, C. L; Magnusdottir, G.; Smyth, P.; Stern, H.

    2010-01-01

    fall over the tropical Pacific ocean during August 1979,the tropical Pacific and Atlantic oceans, J. Clim. , 17,systems over the west Pacific Ocean had two peaks, one at

  7. Larger foraminifer biostratigraphy of PEACE boreholes, Enewetak Atoll, Western Pacific Ocean. Geologic and geophysical investigations of Enewetak Atoll, Republic of the Marshall Islands. Professional paper

    SciTech Connect (OSTI)

    Gibson, T.G.; Margerum, R.

    1991-01-01

    Larger foraminiferal assemblages, including Lepidocyclina orientalis, Miogypsina thecideaeformis, Miogypsinoides dehaartii, etc., and a smaller foraminifer, Austrotrillina striata, are used to correlate upper Oligocene and lower Miocene strata in the Pacific Atoll Exploration Program (PEACE) boreholes at Enewetak Atoll, Republic of the Marshall Islands, western Pacific Ocean, with the Te and Tf zones of the previously established Tertiary Far East Letter Zonation. Correlation using these two benthic groups is critical because calcareous nannofossils and planktic foraminifers are absent in the lower Miocene strata. Biostratigraphic data from these boreholes delineate a thick (greater than 700 feet) sequence of upper Oligocene and lower Miocene strata corresponding to lower and upper Te zone. These strata document a major period of carbonate accumulation at Enewetak during the Late Oligocene and early Miocene (26 to 18 million years ago).

  8. Regional Summary Pacific Management Context

    E-Print Network [OSTI]

    . Bocaccio, Pacific ocean perch, cowcod, and darkblotched and widow rockfish are currently in rebuildingRegional Summary Pacific Management Context The Pacific Region includes California, Oregon, and Washington. Federal fisheries in this region are managed by the Pacific Fishery Management Council (PFMC

  9. Northerly surface wind events over the eastern North Pacific Ocean : spatial distribution, seasonality, atmospheric circulation, and forcing

    E-Print Network [OSTI]

    Taylor, Stephen V.

    2006-01-01

    and C. D. Winant (1995), Buoy observations of the atmosphereQuikSCAT/SeaWinds using ocean buoy data, J. Atmos. Oceanicfield evaluation of NDBC moored buoy winds, J. Atmos. Ocean.

  10. Introduction The Pacific hake (Merluccius produc-

    E-Print Network [OSTI]

    are with Fisheries and Oceans Canada, Pacific Biologi- cal Station, Nanaimo, BC V9T 6N7. Rebecca E. Thomas and Oceans Canada. ABSTRACT--Pacific hake, Merluccius productus, the most abundant groundfish coast, we hypothesize that the annual move- ments of Pacific hake are more responsive to climate-ocean

  11. The distinct behaviors of Pacific and Indian Ocean warm pool properties on seasonal and interannual time scales

    E-Print Network [OSTI]

    Kim, Seon Tae; Yu, Jin-Yi; Lu, Mong-Ming

    2012-01-01

    are there trop- ical warm pools? , J. Clim. , 18, 5294–5331,P. J. Webster (1999), Warm pool SST variability in relationin the western Pacific warm pool, Bull. Am. Meteorol. Soc. ,

  12. STOCK COMPOSITION, GROWTH, MORTALITY, AND AVAILABILITY OF PACIFIC SAURY,

    E-Print Network [OSTI]

    RA, OF THE NORTHEASTERN PACIFIC OCEAN STEVEN E. HUGHES) ABSTRACT Recent international interest in the Pacific saury (C%/ahi" "£lira) resource of the north- eastern Pacific Ocean prompted studies to determine the stock, in the northeastern Pacific Ocean was begun by our laboratory. This study was a direct result of a tenfold decrease

  13. The distinct behaviors of Pacific and Indian Ocean warm pool properties on seasonal and interannual time scales

    E-Print Network [OSTI]

    Kim, Seon Tae; Yu, Jin-Yi; Lu, Mong-Ming

    2012-01-01

    AND INDIAN OCEAN WARM POOL Rayner, N. A. , D. E. Parker, E.Temperature data set (HadISST) [Rayner et al. , 2003], which

  14. A retrospective study of ecosystem effects of the 1976/77 regime shift in the eastern Pacific warm pool

    E-Print Network [OSTI]

    Vilchis, L. Ignacio

    2010-01-01

    tuna in the eastern Pacific Ocean. Inter-Amer. Trop. Tunatuna in the eastern Pacific Ocean. Inter-Amer. Trop. TunaT.P. , 2001. On the Pacific Ocean regime shift. Geophysical

  15. A retrospective study of ecosystem effects of the 1976/77 regime shift in the eastern Pacific warm pool

    E-Print Network [OSTI]

    Vilchis, L. Ignacio

    2010-01-01

    influences surface currents and oceanic upwelling. WithCurrent in the Tropical Pacific Ocean. Journal of Ocean University of Oingdao (Oceanic

  16. A critical evaluation of the upper ocean heat budget in the Climate Forecast System Reanalysis data for the south central equatorial Pacific

    SciTech Connect (OSTI)

    Liu H.; Lin W.; Liu, X.; Zhang, M.

    2011-08-26

    Coupled ocean-atmospheric models suffer from the common bias of a spurious rain belt south of the central equatorial Pacific throughout the year. Observational constraints on key processes responsible for this bias are scarce. The recently available reanalysis from a coupled model system for the National Centers for Environmental Prediction (NCEP) Climate Forecast System Reanalysis (CFSR) data is a potential benchmark for climate models in this region. Its suitability for model evaluation and validation, however, needs to be established. This paper examines the mixed layer heat budget and the ocean surface currents - key factors for the sea surface temperature control in the double Inter-Tropical Convergence Zone in the central Pacific - from 5{sup o}S to 10{sup o}S and 170{sup o}E to 150{sup o}W. Two independent approaches are used. The first approach is through comparison of CFSR data with collocated station observations from field experiments; the second is through the residual analysis of the heat budget of the mixed layer. We show that the CFSR overestimates the net surface flux in this region by 23 W m{sup -2}. The overestimated net surface flux is mainly due to an even larger overestimation of shortwave radiation by 44 W m{sup -2}, which is compensated by a surface latent heat flux overestimated by 14 W m{sup -2}. However, the quality of surface currents and the associated oceanic heat transport in CFSR are not compromised by the surface flux biases, and they agree with the best available estimates. The uncertainties of the observational data from field experiments are also briefly discussed in the present study.

  17. Impacts of the Indian Ocean on the ENSO cycle Jin-Yi Yu, Carlos R. Mechoso, James C. McWilliams, and Akio Arakawa

    E-Print Network [OSTI]

    Yu, Jin-Yi

    , the ocean model domain includes only the tropical Pacific Ocean (the Pacific Run). In the other experiment, the ocean model domain includes both the Indian and tropical Pacific Oceans (the Indo-Pacific Run Oceans tends to be more realistic than that including the tropical Pacific Ocean only. In particular

  18. Sedimentary and mineral dust sources of dissolved iron to the world ocean

    E-Print Network [OSTI]

    Moore, J. K; Braucher, O.

    2008-01-01

    of the tropi- cal Pacific Ocean II. Iron biogeochemistry,in the Northeast Pacific Ocean Gyre: Aerosols, iron, and theF. M. M. : The equatorial Pacific Ocean: Grazer-controlled

  19. The West Pacific diversity hotspot as a source or sink for new species? Population genetic insights from the

    E-Print Network [OSTI]

    Bermingham, Eldredge

    and Central-West Pacific, Hawaii and the Central-West Pacific, and Indian Ocean and the Central-West Pacific-Australian Archipelago (IAA), at the junction of the Indian and Pacific oceans, and declines to both the east Ocean (Briggs 1999). Pleistocene isola- tion of the Pacific and Indian Oceans, driven by +100 m changes

  20. Data report: Oligocene paleoceanography of the equatorial Pacific Ocean: planktonic and benthic stable isotope results from Site 1218 

    E-Print Network [OSTI]

    Wade, Bridget S.; P??like, Heiko

    2005-01-01

    To document the evolution of the early cryosphere, stable isotope analyses were conducted on the planktonic and benthic foraminifers from Ocean Drilling Program Site 1218. We generated two parallel 54- m-long records ...

  1. Mechanisms for the Interannual Variability of SST in the East Pacific Warm Pool KRISTOPHER B. KARNAUSKAS

    E-Print Network [OSTI]

    Karnauskas, Kristopher

    with the western and equatorial Pacific Ocean, relatively little is known about the east Pacific warm pool (EPWP model (OGCM) of the tropical Pacific Ocean and various atmospheric and oceanic observations are used correlation between SST in the EPWP and eastern equatorial Pacific is therefore explained not by ocean

  2. Low-frequency western Pacific Ocean sea level and circulation changes due to the connectivity of the Philippine Archipelago

    E-Print Network [OSTI]

    Qiu, Bo

    of the Philippine Archipelago Wei Zhuang,1 Bo Qiu,2 and Yan Du1 Received 26 August 2013; revised 18 November 2013 changes associated with the oceanic connectivity around the Philippine Archipelago are studied using-driven baroclinic Rossby waves impinge on the eastern Philippine coast and excite coastal Kelvin waves, conveying

  3. Mapping the Potential of U.S. Ocean Energy | Department of Energy

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    undertaken to date to accurately define the magnitude and location of U.S. and global wave, tidal, ocean thermal, and continental U.S. river hydrokinetic resources. With more...

  4. NE Pacific Basin --Tagging Data Kate Myers, Ph.D.

    E-Print Network [OSTI]

    Ocean B: NE Pacific Basin --Tagging Data Kate Myers, Ph.D. Principal Investigator, High Seas Salmon ocean tagging research on Columbia River salmon and steelhead migrating in the NE Pacific Basin R. Basin in 1995-2004. Fisheries and Oceans Canada, Pacific Biological Station, Nanaimo, B

  5. ECOSYSTEM INDICATORS AND TRENDS USED BY FOCI NORTH PACIFIC REGION

    E-Print Network [OSTI]

    of atmospheric forcing and physical oceanographic response of the North Pacific Ocean and Bering Sea Pacific whick is taken as an indicator of a change in the PDO. Ocean temperatures throughout the North temperature variability. The PDO is a long- lived, El Niño-like pattern of North Pacific Ocean climate

  6. International Pacific Research Center October 1997March 2000

    E-Print Network [OSTI]

    Wang, Yuqing

    International Pacific Research Center October 1997­March 2000 School of Ocean and Earth Science #12;International Pacific Research Center October 1997­March 2000 School of Ocean and Earth Science . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .1 Research Activities and Results Theme 1: Indo-Pacific Ocean Climate Overview

  7. Dept. of Ocean and Resources Engineering School of Ocean and Earth Science and Technology

    E-Print Network [OSTI]

    ) Only Indian and Pacific Ocean GlobalEEZ100km from shorelineAtlantic OceanIndo-Pacific #12;OTEC MODELINGDept. of Ocean and Resources Engineering School of Ocean and Earth Science and Technology of deep layers, Increase in THC strength 1) Global 2) EEZ 3)100km from Shoreline 4) Only Atlantic Ocean 5

  8. GROWTH OF PACIFIC SAUR~ COWLABlS SAlRA, IN THE NORTHEASTERN AND NORTHWESTERN PACIFIC OCEANI

    E-Print Network [OSTI]

    the northeastern and northwestern Pacific Ocean was studied using otolith growth increments. We found that growth, Cololabis saira (Brevoort), is distributed throughout the North Pacific Ocean and is one of the most the northwestern Pacific Ocean. Details of sampling and methods of reading otoliths are summarized in Table 1

  9. Primary production in the eastern tropical Pacific: A review J. Timothy Pennington a

    E-Print Network [OSTI]

    Pennington, J. Timothy

    , Peru Abstract The eastern tropical Pacific includes 28 million km2 of ocean between 23.5°N phytoplankton growth (and nitrogen fixation) over large portions of the open-ocean eastern tropical Pacific Pacific. Seasonal cycles are weak over much of the open-ocean eastern tropical Pacific, although several

  10. Habitat and Nursery Grounds of Pacific Rockfish, Sebastes spp., in Rocky

    E-Print Network [OSTI]

    ocean perch, Sebastes alutus, and most other rockfishes, Sebastes spp., in the North Pacific Ocean of southeastern Alaska were important nursery grounds for Pacific ocean perch. These rough areas extend off- shore Pacific ocean perch, have been trawled nearshore in coastal bays and fiords of southeastern Alaska over

  11. Mapping the Potential of U.S. Ocean Energy | Department of Energy

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home Page on Delicious Rank EERE: Alternative Fuelsof EnergyApril 2014 |Department of EnergyMapping the Frontier of New

  12. UH Parking Access & Mid-Pacific Institute

    E-Print Network [OSTI]

    Hall Keller Hall Physical Science Building Pacific Ocean Science & Technology Kuykendall AnnexStairs Pond UH Parking Access & Mid-Pacific Institute Exit M¯anoa Innovation Center and Kau Auxiliary Services Pacific Biomedical Warehouse Agricultural Science Shops Campus Security n Landscaping

  13. UH Parking Access & Mid-Pacific Institute

    E-Print Network [OSTI]

    Hall Keller Hall Physical Science Building Pacific Ocean Science & Technology Kuykendall Annex44 44 Stairs Pond UH Parking Access & Mid-Pacific Institute Exit M¯anoa Innovation Center and Kau Auxiliary Services Pacific Biomedical Warehouse Agricultural Science Shops Campus Security n Landscaping

  14. Facts about ENSO: . Originates in the tropical Pacific

    E-Print Network [OSTI]

    : . Computer models show skill in forecasting tropical Pacific Ocean temperatures one to two years in advance for Pacific Ocean observations that are the foundation of skillful ENSO forecasts: Moored buoys Drifting buoysaaaaaa Facts about ENSO: . Originates in the tropical Pacific . Has a periodicity of 2­7 years

  15. Resources for research Palaeoclimate research in the Pacific

    E-Print Network [OSTI]

    currents flowing into the Coral Sea in the western Pacific. ··· Seismometers on the ocean floor OceanResources for research Palaeoclimate research in the Pacific #12;··· Scientific equipment: pooled Caledonian lagoon and the western Pacific, including the Santo biodiversity survey in Vanuatu. ··· Clinical

  16. Structural and Morphologic Study of Shatsky Rise Oceanic Plateau in the Northwest Pacific Ocean from 2D Multichannel Seismic Reflection and Bathymetry Data and Implications for Oceanic Plateau Evolution 

    E-Print Network [OSTI]

    Zhang, Jinchang

    2014-04-10

    on R/V Marcus G. Langseth during two cruises. The MCS profiles allow us to image Shatsky Rise's upper crustal structure and Moho structure with unprecedented detail, and the multi-beam bathymetry data allow us to produce an improved bathymetric map...

  17. DOI 10.1007/s00382-015-2668-0 Why the South Pacific Convergence Zone is diagonal

    E-Print Network [OSTI]

    Matthews, Adrian

    tropical Pacific Ocean during austral sum- mer (Fig. 1a). The SPCZ is oriented diagonally, stretch- ing northwest­southeast from New Guinea to the central, subtropical Pacific Ocean (Vincent 1994, the majority of precipi- tation over the Pacific Ocean is concentrated in the South Pacific Convergence Zone

  18. International Pacific Research CenterInternational Pacific Research Center April 2000 March 2001 ReportApril 2000 March 2001 Report

    E-Print Network [OSTI]

    Wang, Yuqing

    . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .3 Research Activities and Accomplishments Theme 1: Indo-Pacific Ocean Climate OverviewInternational Pacific Research CenterInternational Pacific Research Center April 2000 ­ March 2001 ReportApril 2000 ­ March 2001 Report School of Ocean and Earth Science and Technology University of Hawai

  19. Diurnal cycle of the Intertropical Convergence Zone in the east Pacific

    E-Print Network [OSTI]

    Bain, C. L; Magnusdottir, G.; Smyth, P.; Stern, H.

    2010-01-01

    over the oceanic warm pool, Mon. Weather Rev. , 121, 1398–the tropical Pacific warm pool, Q. J. R. Meteorol. Soc. ,

  20. IEEE JOURNAL OF OCEANIC ENGINEERING, VOL. 27, NO. 2, APRIL 2002 155 Very High-Frequency Radar Mapping of

    E-Print Network [OSTI]

    Miami, University of

    Weisberg, P. Edgar An, Alexander Soloviev, and Mark Luther Abstract--An ocean surface current radar (OSCR coastal ocean currents over a 7.5 km 8 km domain with a horizontal resolution of 250 m at 700 grid points at the SFOMC. Index Terms--ADCP, coastal ocean circulation, current profiles, surface currents, VHF radar

  1. Pacific bluefin tuna (Thunnus orien-talis), a highly migratory species, is

    E-Print Network [OSTI]

    in the temperate zone of the northern Pacific Ocean (Yamanaka, 1982; Bayliff, 1994) in con- trast to T. thynnus, which inhabits the Atlantic Ocean (Collette, 1999). Current knowledge on the migration of Pacific in the northwest Pacific Ocean in an area from the Philippines past Taiwan to Okinawa from April to June, and small

  2. An investigation of the relationships between rainfall in northeast Brazil and sea surface temperatures of the equatorial regions of the Pacific and Atlantic Oceans 

    E-Print Network [OSTI]

    Cochrane, Marvin Arthur

    1977-01-01

    N RA INFALL IiN NORTHEAST DPA: IL AND SLiA SUR!'ACE TEMPLRATUiRIiS Ol' THE EQUATORIAL RFU!ONS JF THE PACIFIC AND ATl. ANTIC OCFANS A Thesrs by iKKRVTN ARTHUR COCHRAiNE Approved as to style and coiitent by: (Cha i r;iian o F !;e mnittce) (i.... TABLE OF CONTENTS ABSTRACT Page ACKNOWI, EDGI'. MFNTS I. IST OF TABLES LIST OF FIGURLS 1V V11 , V11 1 1. INTRODUCTION a. General b. Ol&jcctivcs 2. LITEIIATURL' REVIEW a. Iforf. beast Brazi I rainfall ? equatorial Pacific SST b . Ilortheast...

  3. Maps

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantity of NaturalDukeWakefieldSulfateSciTechtail.Theory ofDid you notHeat PumpsTechnologiesTechnologiesScience & InnovationMaps

  4. MAP

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantity ofkandz-cm11 Outreach Home Room NewsInformationJesse BergkampCentermillion to localPartnership willLynn Rippe2D,MANTISSA DayMAP

  5. Maps

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantityBonneville Power Administration would likeUniverseIMPACTThousandReport)PriceHistoricEnergy EfficiencyMaps Sign In About |

  6. LEG 142 PRELIMINARY REPORT OCEAN DRILLING PROGRAM

    E-Print Network [OSTI]

    LEG 142 PRELIMINARY REPORT OCEAN DRILLING PROGRAM ENGINEERING PRELIMINARY REPORT NO. 3 EAST PACIFIC RISE 1992 #12;OCEAN DRILLING PROGRAM LEG 142 PRELIMINARY REPORT East Pacific Rise Dr. Rodey Batiza Co 96822 Mr. Michael A. Storms Operations Superintendent/ Assistant Manager of Engineering and Drilling

  7. Ocean Sci., 6, 775787, 2010 www.ocean-sci.net/6/775/2010/

    E-Print Network [OSTI]

    in the Pacific Ocean F. M. Bingham1, G. R. Foltz2, and M. J. McPhaden3 1Center for Marine Science, Univ. of North salinity (SLS) is examined in the Pacific Ocean between 40 S and 60 N using a variety of data sourcesOcean Sci., 6, 775­787, 2010 www.ocean-sci.net/6/775/2010/ doi:10.5194/os-6-775-2010 © Author

  8. Predictability and Diagnosis of Low Frequency Climate Processes in the Pacific, Final Technical Report

    SciTech Connect (OSTI)

    Niklas Schneider

    2009-06-17

    The report summarized recent findings with respect to Predictability and Diagnosis of Low Frequency Climate Processes in the Pacific, with focus on the dynamics of the Pacific Decadal Oscillation, oceanic adjustments and the coupled feedback in the western boundary current of the North and South Pacific, decadal dynamics of oceanic salinity, and tropical processes with emphasis on the Indonesian Throughflow.

  9. Calcareous nannofossils and planktic foraminifers from Enewetak Atoll, Western Pacific Ocean: Geologic and geophysical investigations of Enewetak Atoll, Republic of the Marshall Islands. Professional paper

    SciTech Connect (OSTI)

    Bybell, L.M.; Poore, R.Z.

    1991-01-01

    Boring of the carbonate sequence at the northern end of Enewetak Atoll, Republic of the Marshall Islands, was conducted in 1985, as part of the Pacific Enewetak Atoll Crater Exploration (PEACE) Program. The overall goal of the program was to characterize physical effects of large-scale nuclear blasts, which were conducted in the early 1950's, on the sediments of the atoll. In the report the authors document the occurrences of stratigraphically diagnostic planktic microfossils in samples from Enewetak (generally referred to as core) and outline the rationale for incorporating all available diagnostic planktic assemblages into a composite sequence that was used to date the Enewetak benthic zonation.

  10. ''A ground water resources study of a Pacific Ocean atoll - Tarawa, Gilbert Islands,'' by J. W. Lloyd, J. C. Miles, G. R. Chessmand, and S. F. Bugg

    SciTech Connect (OSTI)

    Wheatcraft, S.W.; Buddemeier, R.W.

    1981-10-01

    Several inherent problems in the methodology employed in the ground water resource study of Tarawa Atoll (Lloyd, et al., 1981) are described. Studies of Enewetak Atoll have provided data that require a significantly different conceptual model of the atoll hydrogeology system. Comparison of well, lagoon, and ocean tidal observations with a mathematical model that assumes horizontal tidal propagation indicates that the observed results are more consistent with a system that is controlled by vertical coupling between the unconsolidated surface aquifer and an underlying aquifer of more permeable limestone. This indicates that most fresh water recharged to the aquifer migrates downward and mixes with the sea water in a deeper aquifer providing easy exchange with the ocean. Lloyd, et al., do not take tidal mixing or vertical transport into account and it therefore seems likely that fresh water inventories are significantly overestimated. Failure to include these significant loss terms in the island water budget may also account for calculated heads above ground level. (JMT)

  11. Regional Patterns of Tropical Indo-Pacific Climate Change: Evidence of the Walker Circulation Weakening*

    E-Print Network [OSTI]

    Xie, Shang-Ping

    in the tropical eastern Pacific and western Indian Ocean than in the tropical western Pacific and eastern IndianRegional Patterns of Tropical Indo-Pacific Climate Change: Evidence of the Walker Circulation Weakening* HIROKI TOKINAGA, SHANG-PING XIE, AND AXEL TIMMERMANN International Pacific Research Center, SOEST

  12. Lead Isotopic Variations of the Pacific and Implications for Paleogene Water Mass Composition 

    E-Print Network [OSTI]

    Subt, Cristina

    2013-11-13

    meridional temperature gradients. Nd isotopes indicate high-latitude convection in the Pacific Ocean during this interval, with deep waters mixing in the tropical Pacific. Here we investigate the evolution of the Pb isotopic composition of water masses...

  13. OCEAN DRILLING PROGRAM LEG 202 SCIENTIFIC PROSPECTUS

    E-Print Network [OSTI]

    OCEAN DRILLING PROGRAM LEG 202 SCIENTIFIC PROSPECTUS SOUTHEAST PACIFIC PALEOCEANOGRAPHIC TRANSECTS __________________ Dr. Jack Baldauf Deputy Director of Science Operations Ocean Drilling Program Texas A&M University Manager and Staff Scientist Ocean Drilling Program Texas A&M University 1000 Discovery Drive College

  14. PAC I F I C C OAS T S A L M O N Pacific Coast Salmon

    E-Print Network [OSTI]

    recreationally and commercially in the Pacific Ocean, Puget Sound, and in freshwater rivers on their spawning of gear depending on location: in the Pacific Ocean all harvest is by trolling; in Puget Sound, gillnetsPAC I F I C C OAS T S A L M O N 1 U N I T 12 Pacific Coast Salmon Unit 12 ROBERT G. KOPE NMFS

  15. Tidal-Fluvial and Estuarine Processes in the Lower Columbia River: I. Along-channel Water Level Variations, Pacific Ocean to Bonneville Dam

    SciTech Connect (OSTI)

    Jay, D. A.; Leffler, K.; Diefenderfer, Heida L.; Borde, Amy B.

    2014-06-07

    This two-part paper provides comprehensive time and frequency domain analyses and models of along-channel water level variations in the 234km-long Lower Columbia River and Estuary (LCRE) and documents the response of floodplain wetlands thereto. In Part I, power spectra, continuous wavelet transforms, and harmonic analyses are used to understand the influences of tides, river flow, upwelling and downwelling, and hydropower operations ("power-peaking") on the water level regime. Estuarine water levels are influenced primarily by astronomical tides and coastal processes, and secondarily by river flow. The importance of coastal and tidal influences decreases in the landward direction, and water levels are increasingly controlled by river flow variations at periods from ?1day to years. Water level records are only slightly non-stationary near the ocean, but become increasingly irregular upriver. Although astronomically forced tidal constituents decrease above the estuary, tidal fortnightly and overtide variations increase for 80-200km landward, both relative to major tidal constituents and in absolute terms.

  16. The Cold Dark Ocean This talk will help younger students understand that most of the ocean is an expansive cold

    E-Print Network [OSTI]

    to the El Niño/La Niña cycle in the Pacific Ocean and how it impacts the climate of the Southeast UThe Cold Dark Ocean This talk will help younger students understand that most of the ocean is an expansive cold dark abyss. The concepts of solar heating of the ocean surface and effects of temperature

  17. Carbon dioxide, hydrographic, and chemical data obtained in the Central South Pacific Ocean (WOCE sections P17S and P16S) during the tunes-2-expedition of the R/V Thomas Washington, July--August 1991

    SciTech Connect (OSTI)

    1991-12-31

    This data documentation discusses the procedures and methods used to measure total carbon dioxide (TCO{sub 2}), discrete partial pressure of TCO{sub 2} (pCO{sub 2}), and total alkalinity (TALK), during the Research Vessel (R/V) Thomas Washington TUNES Leg 2 Expedition in the central South Pacific Ocean. Conducted as part of the World Ocean Circulation Experiment (WOCE), the cruise began in Papeete, Tahiti, French Polynesia, on July 16, 1991, and returned to Papeete on August 25, 1991. WOCE Meridional Sections P17S along 135{degrees} W and P16S along 150{degrees} W were completed during the 40-day expedition. A total of 97 hydrographic stations were occupied. Hydrographic and chemical measurements made along WOCE Sections P17S and P16S included pressure, temperature, salinity, and oxygen measured by conductivity, temperature and depth sensor; bottle salinity; oxygen; phosphate; nitrate; nitrite; silicate; CFC-12; CFC- 11; TCO{sub 2}; TALK; and pCO{sub 2} measured at 20{degrees}C. The TCO{sub 2} concentration in 1000 seawater samples was determined with a coulometric analysis system, the pCO{sub 2} in 940 water samples was determined with an equilibrator/gas chromatograph system, while the TALK concentration in 139 samples was determined on shore at the laboratory of C. Goyet of Woods Hole Oceanographic Institution with an alkalinity titration system. In addition, 156 coulometric measurements for the Certified Reference Material (Batch {number_sign}6) were made and yielded a mean value of 2303.2 {plus_minus} 1.5 {mu}mol/kg. This mean value agrees within a standard deviation of the 2304.6 {plus_minus} 1.6 {mu}mol/kg (N=9) value determined with the manometer of C. D. Keeling at Scripps Institution of Oceanography (SIO). Replicate samples from 11 Niskin bottles at 4 stations were also collected for later shore-based reference analyses of TCO{sub 2} and TALK by vacuum extraction and manometry in the laboratory of C. D. Keeling of SIO.

  18. Eddy-Induced Heat Transport in the Subtropical North Pacific from Argo, TMI, and Altimetry Measurements

    E-Print Network [OSTI]

    Qiu, Bo

    Eddy-Induced Heat Transport in the Subtropical North Pacific from Argo, TMI, and Altimetry transport induced by mesoscale oceanic eddies is estimated by combining satellite- derived sea surface temperature­salinity data. In the North Pacific Ocean subtropical gyre, warm (cold) temperature anomalies

  19. Cooling history of the Pacific lithosphere Michael H. Ritzwoller*, Nikolai M. Shapiro, Shi-Jie Zhong

    E-Print Network [OSTI]

    Shapiro, Nikolai

    Cooling history of the Pacific lithosphere Michael H. Ritzwoller*, Nikolai M. Shapiro, Shi or blithosphereQ forms and thickens as the plate cools during its journey away from mid-ocean ridges. Numerous, particularly across the Pacific, does not cool continuously as it ages. Based on a seismic model of the Pacific

  20. Nitrogen uptake by plants subsidized by Pacific salmon carcasses: a hierarchical experiment

    E-Print Network [OSTI]

    Reynolds, John D.

    the Pacific Rim. Salmon are born in freshwater, with most popu- lations migrating as juveniles to the oceanNitrogen uptake by plants subsidized by Pacific salmon carcasses: a hierarchical experiment Morgan and transport large numbers of Pacific salmon (Oncorhynchus spp.) to riparian areas beside small coastal streams

  1. Walleye pollock (Theragra chalcogram-ma) and Pacific herring (Clupea pallasi)

    E-Print Network [OSTI]

    that inhabit the north- eastern Pacific Ocean rim. Both species are important components of marine bird, mammal482 Walleye pollock (Theragra chalcogram- ma) and Pacific herring (Clupea pallasi) are forage fish and Speckman, 1997;Anderson and Piatt,1999).Young- of-the-year (YOY) walleye pollock and YOY Pacific herring

  2. OCEAN DRILLING PROGRAM LEG 202 SCIENTIFIC PROSPECTUS

    E-Print Network [OSTI]

    OCEAN DRILLING PROGRAM LEG 202 SCIENTIFIC PROSPECTUS SOUTHEAST PACIFIC PALEOCEANOGRAPHIC TRANSECTS, this source should be appropriately acknowledged. Ocean Drilling Program Scientific Prospectus No. 102 Publications homepage on the World Wide Web at: http://www-odp.tamu.edu/publications This publication

  3. OCEAN DRILLING PROGRAM LEG 132 PRELIMINARY REPORT

    E-Print Network [OSTI]

    OCEAN DRILLING PROGRAM LEG 132 PRELIMINARY REPORT ENGINEERING II: WESTERN AND CENTRAL PACIFIC Mr. Michael A. Storms Supervisor of Development Engineering Ocean Drilling Program Texas A&M University and Drilling Operations ODP/TAMU Timothy J.G. Francis Deputy Director ODP/TAMU September 1990 #12;This informal

  4. OCEAN DRILLING PROGRAM LEG 191 SCIENTIFIC PROSPECTUS

    E-Print Network [OSTI]

    OCEAN DRILLING PROGRAM LEG 191 SCIENTIFIC PROSPECTUS NORTHWEST PACIFIC SEISMIC OBSERVATORY AND HAMMER DRILL ENGINEERING TESTS Dr. Toshihiko Kanazawa Co-Chief Scientist Earthquake Research Institute Director of Science Operations Ocean Drilling Program Texas A&M University 1000 Discovery Drive College

  5. Air-sea interaction at contrasting sites in the Eastern Tropical Pacific : mesoscale variability and atmospheric convection at 10°N

    E-Print Network [OSTI]

    Farrar, J. Thomas (John Thomas), 1976-

    2007-01-01

    The role of ocean dynamics in driving air-sea interaction is examined at two contrasting sites on 125°W in the eastern tropical Pacific Ocean using data from the Pan American Climate Study (PACS) field program. Analysis ...

  6. Ocean Salmon Ranching in the North Pacific

    E-Print Network [OSTI]

    Fucile, Mark J.

    1982-01-01

    chum salmon returning to Sakhalin. . . show that an averagegained complete control of Sakhalin. A. NETBOY, supra notethe south- ern portion of Sakhalin to Japan. Id. 143. Areas

  7. Nitrite dynamics in the open ocean - clues from seasonal and diurnal variations

    E-Print Network [OSTI]

    2012-01-01

    2009, Paytan et al. 2009, Wankel et al. 2010). The conservedPacific Ocean. Limnol Oceanogr Wankel SD, Chen Y, Kendall C,

  8. Impacts of increasing anthropogenic soluble iron and nitrogen deposition on ocean biogeochemistry

    E-Print Network [OSTI]

    2009-01-01

    some increased CO 2 outgassing in the equatorial Pacific. [estimated oceanic O 2 outgassing associated to global warm-increased oceanic O 2 outgassing by $10 Tmol O 2 /a in the

  9. Compound-Specific Radiocarbon Analyses of Phospholipid Fatty Acids and n-Alkanes in Ocean Sediments

    E-Print Network [OSTI]

    2010-01-01

    Monica Basin surface sediment: a model based on compound-ACIDS AND n-ALKANES IN OCEAN SEDIMENTS Ellen R M Druffel 1 •organic matter in ocean sediments from the northeast Pacific

  10.  COMPOUND-SPECIFIC RADIOCARBON ANALYSES OF PHOSPHOLIPID FATTY ACIDS AND n -ALKANES IN OCEAN SEDIMENTS

    E-Print Network [OSTI]

    2010-01-01

    Monica Basin surface sediment: a model based on compound-ACIDS AND n-ALKANES IN OCEAN SEDIMENTS Ellen R M Druffel 1 •organic matter in ocean sediments from the northeast Pacific

  11. Effects of internal waves on low frequency, long range, acoustic propagation in the deep ocean

    E-Print Network [OSTI]

    Xu, Jinshan

    2007-01-01

    This thesis covers a comprehensive analysis of long-range, deep-ocean, low-frequency, sound propagation experimental results obtained from the North Pacific Ocean. The statistics of acoustic fields after propagation through ...

  12. Pacific Island Energy Snapshots

    Broader source: Energy.gov [DOE]

    These energy snapshots highlight the energy landscape of islands in the Pacific and the surrounding area.

  13. PACIFIC SOUTHWEST FOREST SERVICE

    E-Print Network [OSTI]

    Columbia, Canada. ACKNOWLEDGMENTS I thank Lula E. Greene, Pacific Southwest Forest and Range Experi ment

  14. Activity Stream - Mapping and Assessment of the United States...

    Open Energy Info (EERE)

    Mapping and Assessment of the United States Ocean Wave Energy Resource 8 months ago Jay Huggins updated the dataset Mapping and Assessment of the United States Ocean Wave Energy...

  15. Central Equatorial Pacific Experiment (CEPEX)

    SciTech Connect (OSTI)

    Not Available

    1993-01-01

    The Earth's climate has varied significantly in the past, yet climate records reveal that in the tropics, sea surface temperatures seem to have been remarkably stable, varying by less than a few degrees Celsius over geologic time. Today, the large warm pool of the western Pacific shows similar characteristics. Its surface temperature always exceeds 27[degree]C, but never 31[degree]C. Heightened interest in this observation has been stimulated by questions of global climate change and the exploration of stabilizing climate feedback processes. Efforts to understand the observed weak sensitivity of tropical sea surface temperatures to climate forcing has led to a number of competing ideas about the nature of this apparent thermostat. Although there remains disagreement on the processes that regulate tropical sea surface temperature, most agree that further progress in resolving these differences requires comprehensive field observations of three-dimensional water vapor concentrations, solar and infrared radiative fluxes, surface fluxes of heat and water vapor, and cloud microphysical properties. This document describes the Central Equatorial Pacific Experiment (CEPEX) plan to collect such observations over the central equatorial Pacific Ocean during March of 1993.

  16. Lagrangian tools to monitor transport and mixing in the ocean

    E-Print Network [OSTI]

    S. V. Prants; M. V. Budyansky; M. Yu. Uleysky

    2012-05-20

    We apply the Lagrangian approach to study surface transport and mixing in the ocean. New tools have been developed to track the motion of water masses, their origin and fate and to quantify transport and mixing. To illustrate the methods used we compute the Lagrangian synoptic maps a comparatively small marine bay, the Peter the Great Bay in the Japan Sea near Vladivostok city (Russia), and in a comparatively large region in the North Pacific, the Kuroshio Extension system. In the first case we use velocity data from a Japan Sea circulation numerical model and in the second one the velocity data are derived from satellite altimeter measurements of anomalies of the sea height distributed by AVISO.

  17. 90E 120 150 180 210 240 270 300 330 0 30 60 OCEAN ATLANTIC

    E-Print Network [OSTI]

    GREENLAND EUROPE AFRICA SOUTH AMERICA NORTH AMERICA ASIA AUSTRALIA ANTARCTICA INDIAN OCEAN PACIFIC OCEAN ATLANTIC OCEAN ARCTIC OCEAN 418 625 626-636 637-641 642-644 645 646 647 648-649 650-656 657-659 660-661 662 1102-1103 1104-1106 1107 1108-1118 1119 1120 1121 1122 1123 1124 1125 1126-1134 998-1001 SOUTHERN OCEAN

  18. OCEAN DRILLING PROGRAM LEG 142 ENGINEERING AND SCIENTIFIC PROSPECTUS

    E-Print Network [OSTI]

    OCEAN DRILLING PROGRAM LEG 142 ENGINEERING AND SCIENTIFIC PROSPECTUS EAST PACIFIC RISE Mr. Michael A. Storms Operations Superintendent/ Assistant Manager of Engineering and Drilling Operations Ocean Drilling Program Texas A&M University Research Park 1000 Discovery Drive College Station, Texas 77845

  19. Natural Radiocarbon Distribution in the Deep Ocean Katsumi MATSUMOTO1

    E-Print Network [OSTI]

    Matsumoto, Katsumi

    , World Ocean Circulation Experiment (WOCE), ocean ventilation, North Atlantic Deep Water, Antarctic Bottom Water, Circumpolar Deep Water, Pacific Deep Water, thermohaline circulation 1. INTRODUCTION Deep in the subtropical North Atlantic, revealed that much of the deep water is cold, and warm water is confined to a thin

  20. OCEAN DRILLING PROGRAM LEG 181 SCIENTIFIC PROSPECTUS

    E-Print Network [OSTI]

    OCEAN DRILLING PROGRAM LEG 181 SCIENTIFIC PROSPECTUS SOUTHWEST PACIFIC GATEWAYS Dr. Robert M acknowledgment of this source. Scientific Prospectus No. 81 First Printing 1998 Distribution Electronic copies of this publication may be obtained from the ODP Publications Home Page on the World Wide Web at http

  1. Mid-ocean microseisms Peter D. Bromirski

    E-Print Network [OSTI]

    Bromirski, Peter D.

    , and the Hawaiian Islands appear to be a significant source of LPDF energy in the North Pacific when waves arrive peak, is caused by ocean wave energy couplin Sciences and Technology, University of Hawaii, Honolulu, Hawaii 96822, USA (fkd@hawaii.edu) Ralph A

  2. Ocean response to arbitrary wind perturbations in the low-frequency approximation: implications for ENSO and

    E-Print Network [OSTI]

    expansion about a small parameter that involves the dominant frequency of the wind forcing and the oceanic1 Ocean response to arbitrary wind perturbations in the low-frequency approximation: implications study the response of the ocean thermocline in the Pacific to arbitrary periodic wind stress

  3. Hybrid coupled models of the tropical Pacific: I interannual variability

    E-Print Network [OSTI]

    Tang, Youmin

    Y. Tang Hybrid coupled models of the tropical Pacific: I interannual variability Received: 20 Two hybrid coupled models (HCMs), an intermediate complexity dynamical ocean model cou- pled to either), hybrid models (e.g., Barnett et al. 1993; Balmaseda et al. 1994,1995), and fully coupled general

  4. Tropical Pacific mid-latitude teleconnections in medieval times

    E-Print Network [OSTI]

    Cobb, Kim

    records from widely distributed regions around the planet, and in many cases is consistent with a cool centennial-scale drought, elevated incidence of wild fire, cool sea surface temperatures (SSTs) along). Proxy records from the tropical Pacific Ocean show contemporaneous changes indicating cool central

  5. Skipjack tuna, Katsuwonus pelamis, are distributed throughout the Pacific

    E-Print Network [OSTI]

    343 Skipjack tuna, Katsuwonus pelamis, are distributed throughout the Pacific Ocean in tropical at processing plants in Manta (Ecuador), Assessment of skipjack tuna (Katsuwonus pelamis) spawning activity 2000. Fish. Bull. 99:343­350 (2001). Abstract­An investigation of skip- jack tuna, Katsuwonus pelamis

  6. THE INTERNATIONAL PACIFIC RESEARCH CENTER 1 PUBLICATIONS 3

    E-Print Network [OSTI]

    Wang, Yuqing

    the School of Ocean and Earth Science and Technology at the University of Hawai`i at Mänoa. The IPRC mission of the nature and predict- ability of climate variations and change in the Asia- Pacific region: the Japan Agency for Marine- Earth Science and Technology (JAMSTEC), NASA and NOAA. Financial support

  7. PACIFIC NORTHWEST CYBER SUMMIT

    SciTech Connect (OSTI)

    Lesperance, Ann M.; Matlock, Gordon W.; Becker-Dippmann, Angela S.; Smith, Karen S.

    2013-08-07

    On March 26, 2013, the Snohomish County Public Utility District (PUD) and the U.S. Department of Energy’s (DOE’s) Pacific Northwest National Laboratory (PNNL) jointly hosted the Pacific Northwest Cyber Summit with the DOE’s Office of Electricity Delivery and Energy Reliability, the White House, Washington State congressional delegation, Washington State National Guard, and regional energy companies.

  8. Migration for Environmentally Displaced Pacific Peoples: Legal Options in the Pacific Rim

    E-Print Network [OSTI]

    Tabucanon, Gil Marvel

    2012-01-01

    the four above-mentioned Pacific Rim states have developedand interests of these Pacific Rim states, but it is alsothe Pacific. All four Pacific Rim countries discussed in

  9. Development of a Species Distribution Model for the East Pacific Green Sea Turtle using Ecological Geoprocessing Tools 

    E-Print Network [OSTI]

    Duncan, Roxanne

    2012-10-19

    East Pacific green sea turtles, Chelonia mydas, play ecologically important roles in marine habitats which range from grazing (and thus regularly "mowing") algae and seagrass beds to cycling nutrients between the ocean and land. However...

  10. A very oligotrophic zone observed from space in the equatorial Pacific warm pool1 Marie-Hlne Radenaca

    E-Print Network [OSTI]

    Boyer, Edmond

    penetration of nutrient-rich water due to the following processes. 1/ The34 equatorial oligotrophic warm pool tropical Pacific, and especially the eastern part of the warm pool,51 is one of the world ocean regions

  11. Comprehensive Ocean Drilling

    E-Print Network [OSTI]

    Comprehensive Ocean Drilling Bibliography containing citations related to the Deep Sea Drilling Project, Ocean Drilling Program, Integrated Ocean Drilling Program, and International Ocean Discovery Program Last updated: May 2014 #12;Comprehensive Bibliography Comprehensive Ocean Drilling Bibliography

  12. Anatomy and evolution of a cyclonic mesoscale eddy observed in the northeastern Pacific tropical-subtropical transition zone

    E-Print Network [OSTI]

    Anatomy and evolution of a cyclonic mesoscale eddy observed in the northeastern Pacific tropical and evolution of a cyclonic mesoscale eddy observed in the northeastern Pacific tropical-subtropical transition zone, J. Geophys. Res. Oceans, 118, doi:10.1002/ 2013JC009339. 1. Introduction [2] Mesoscale eddy

  13. INTERNATIONAL PACIFIC RESEARCH CENTER

    E-Print Network [OSTI]

    Wang, Yuqing

    Center (IPRC) conducts such research, with emphasis on climate variability and change in the Asia-Pacific Data-Research Center . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 57 INTRODUCING with scientists at the Frontier Research Center for Global Change. This model captures such salient features

  14. Drake passage and central american seaway controls on the distribution of the oceanic carbon reservoir

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Fyke, Jeremy G.; D'Orgeville, Marc; Weaver, Andrew J.

    2015-05-01

    A coupled carbon/climate model is used to explore the impact of Drake Passage opening and Central American Seaway closure on the distribution of carbon in the global oceans. We find that gateway evolution likely played an important role in setting the modern day distribution of oceanic dissolved inorganic carbon (DIC), which is currently characterized by relatively low concentrations in the Atlantic ocean, and high concentrations in the Southern, Indian, and Pacific oceans. In agreement with previous studies, we find a closed Drake Passage in the presence of an open Central American Seaway results in suppressed Atlantic meridional overturning and enhancedmore »southern hemispheric deep convection. Opening of the Drake Passage triggers Antarctic Circumpolar Current flow and a weak Atlantic meridional overturning circulation (AMOC). Subsequent Central American Seaway closure reinforces the AMOC while also stagnating equatorial Pacific subsurface waters. These gateway-derived oceanographic changes are reflected in large shifts to the global distribution of DIC. An initially closed Drake Passage results in high DIC concentrations in the Atlantic and Arctic oceans, and lower DIC concentrations in the Pacific/Indian/Southern oceans. Opening Drake Passage reverses this gradient by lowering mid-depth Atlantic and Arctic DIC concentrations and raising deep Pacific/Indian/Southern Ocean DIC concentrations. Central American Seaway closure further reinforces this trend through additional Atlantic mid-depth DIC decreases, as well as Pacific mid-depth DIC concentration increases, with the net effect being a transition to a modern distribution of oceanic DIC.« less

  15. Task 3: PNNL Visit by JAEA Researchers to Participate in TODAM Code Applications to Fukushima Rivers and to Evaluate the Feasibility of Adaptation of FLESCOT Code to Simulate Radionuclide Transport in the Pacific Ocean Coastal Water Around Fukushima

    SciTech Connect (OSTI)

    Onishi, Yasuo

    2013-03-29

    Four JAEA researchers visited PNNL for two weeks in February, 2013 to learn the PNNL-developed, unsteady, one-dimensional, river model, TODAM and the PNNL-developed, time-dependent, three dimensional, coastal water model, FLESCOT. These codes predict sediment and contaminant concentrations by accounting sediment-radionuclide interactions, e.g., adsorption/desorption and transport-deposition-resuspension of sediment-sorbed radionuclides. The objective of the river and coastal water modeling is to simulate • 134Cs and 137Cs migration in Fukushima rivers and the coastal water, and • their accumulation in the river and ocean bed along the Fukushima coast. Forecasting the future cesium behavior in the river and coastal water under various scenarios would enable JAEA to assess the effectiveness of various on-land remediation activities and if required, possible river and coastal water clean-up operations to reduce the contamination of the river and coastal water, agricultural products, fish and other aquatic biota. PNNL presented the following during the JAEA visit to PNNL: • TODAM and FLESCOT’s theories and mathematical formulations • TODAM and FLESCOT model structures • Past TODAM and FLESCOT applications • Demonstrating these two codes' capabilities by applying them to simple hypothetical river and coastal water cases. • Initial application of TODAM to the Ukedo River in Fukushima and JAEA researchers' participation in its modeling. PNNL also presented the relevant topics relevant to Fukushima environmental assessment and remediation, including • PNNL molecular modeling and EMSL computer facilities • Cesium adsorption/desorption characteristics • Experiences of connecting molecular science research results to macro model applications to the environment • EMSL tour • Hanford Site road tour. PNNL and JAEA also developed future course of actions for joint research projects on the Fukushima environmental and remediation assessments.

  16. PUBLISHED ONLINE: 1 APRIL 2012 | DOI: 10.1038/NCLIMATE1461 135 years of global ocean warming between the

    E-Print Network [OSTI]

    Riser, Stephen C.

    of global warming. Warming in the Atlantic Ocean is stronger than in the Pacific. Systematic errors and indicates that globally the oceans have been warming at least since the late-nineteenth or earlyLETTERS PUBLISHED ONLINE: 1 APRIL 2012 | DOI: 10.1038/NCLIMATE1461 135 years of global ocean

  17. ISBN: 978-0-12-391851-2 "Ocean Circulation and Climate, 2nd Ed. A 21st century perspective"

    E-Print Network [OSTI]

    Qiu, Bo

    , persistent currents along the western boundaries of the world's major ocean basins are called "western Australian Current in the Pacific Ocean. Keywords Western boundary current, Gulf Stream, Brazil Current, persistent currents along the western boundaries of the world's major ocean basins are some of the most

  18. S53juNE 2010STATE OFTHE CLIMATE IN 2009 | 3. GLOBAL OCEANS--J. M. Levy, ed.

    E-Print Network [OSTI]

    Khatiwala, Samar

    's energy budget. · Ocean heat fluxes played a dual role in the dynamics of large-scale SST anomalies Niño a considerable build up of heat was observed in the upper equatorial Pacific Ocean. Global integrals of upper-ocean heat content for the last several years have reached values consistently higher

  19. S53JULY 2010STATE OFTHE CLIMATE IN 2009 | 3. Global oceans--J. M. Levy, Ed.

    E-Print Network [OSTI]

    's energy budget. · Ocean heat fluxes played a dual role in the dynamics of large-scale SST anomalies. Heat Niño a considerable build up of heat was observed in the upper equatorial Pacific Ocean. Global integrals of upper-ocean heat content for the last several years have reached values consistently higher

  20. Central Equatorial Pacific Experiment (CEPEX). Design document

    SciTech Connect (OSTI)

    Not Available

    1993-04-01

    The Earth`s climate has varied significantly in the past, yet climate records reveal that in the tropics, sea surface temperatures seem to have been remarkably stable, varying by less than a few degrees Celsius over geologic time. Today, the large warm pool of the western Pacific shows similar characteristics. Its surface temperature always exceeds 27{degree}C, but never 31{degree}C. Heightened interest in this observation has been stimulated by questions of global climate change and the exploration of stabilizing climate feedback processes. Efforts to understand the observed weak sensitivity of tropical sea surface temperatures to climate forcing has led to a number of competing ideas about the nature of this apparent thermostat. Although there remains disagreement on the processes that regulate tropical sea surface temperature, most agree that further progress in resolving these differences requires comprehensive field observations of three-dimensional water vapor concentrations, solar and infrared radiative fluxes, surface fluxes of heat and water vapor, and cloud microphysical properties. This document describes the Central Equatorial Pacific Experiment (CEPEX) plan to collect such observations over the central equatorial Pacific Ocean during March of 1993.

  1. National Oceanic and Atmospheric Administration U.S. Department of Commerce

    E-Print Network [OSTI]

    science, for analyzing current and anticipated uses of ocean, coastal, and Great Lakes areas. Coastal) #12;4 Ocean Uses Assessments ­ Maps and analyzes current and likely future ocean uses by kindsNational Oceanic and Atmospheric Administration U.S. Department of Commerce NOAAStrategic

  2. Pacific Biodiesel: Renewable and Sustainable

    Broader source: Energy.gov [DOE]

    Presentation covers the Pacific Biodiesel topic and is given at the Spring 2011 Federal Utility Partnership Working Group (FUPWG) meeting.

  3. PACIFIC SOUTHWESTt (-A FOREST SERVICE

    E-Print Network [OSTI]

    - ment in 1964. ACKNOWLEDGMENTS We thank Lula E. Greene and the biometries staff of the Pacific Southwest

  4. An Atlantic-Pacific ventilation seesaw across the last deglaciation

    E-Print Network [OSTI]

    Freeman, E.; Skinner, L. C.; Tisserand, A.; Dokken, T.; Timmermann, A.; Menviel, L.; Friedrich, T.

    2015-06-03

    picked and graphitized in the Godwin Labora- ry at the University of Cambridge using a standard hydrogen/iron talyst reduction method (Vogel et al., 1984). For some samples was necessary to combine benthic foraminifera from two adja- nt samples... . Radiocarbon age anomaly at intermediate water depth in the Pacific Ocean during the last deglaciation. Paleoceanography 24 (2223). Stott, L., Timmermann, A., 2011. Hypothesized link between glacial/interglacial at- mospheric CO2 cycles and storage...

  5. Central American geologic map project

    SciTech Connect (OSTI)

    Dengo, G.

    1986-07-01

    During the Northeast Quadrant Panel meeting of the Circum-Pacific Map Project held in Mexico City, February 1985, Central American panel members proposed and adopted plans for compiling a geologic map of Central America, probably at a scale of 1:500,000. A local group with participants from each country was organized and coordinated by Rolando Castillo, director, Central American School of Geology, University of Costa Rica, for the geologic aspects, and Fernando Rudin, director, Geographic Institute of Costa Rica, for the topographic base. In 1956, the US Geological Survey published a geologic map of the region at a scale of 1:1 million. Subsequent topographic and geologic mapping projects have provided a large amount of new data. The entire area is now covered by topographic maps at a scale of 1:50,000, and these maps have been used in several countries as a base for geologic mapping. Another regional map, the Metallogenic Map of Central America (scale = 1:2 million), was published in 1969 by the Central American Research Institute for Industry (ICAITI) with a generalized but updated geologic base map. Between 1969 and 1980, maps for each country were published by local institutions: Guatemala-Belize at 1:500,000, Honduras at 1:500,000, El Salvador at 1:100,000, Nicaragua at 1:1 million, Costa Rica at 1:200,000, and Panama at 1:1 million. This information, in addition to that of newly mapped areas, served as the base for the Central American part of the Geologic-Tectonic Map of the Caribbean Region (scale = 1:2.5 million), published by the US Geological Survey in 1980, and also fro the Northeast Quadrant Maps of the Circum-Pacific Region. The new project also involves bathymetric and geologic mapping of the Pacific and Caribbean margins of the Central American Isthmus. A substantial amount of new information of the Middle America Trench has been acquired through DSDP Legs 67 and 84.

  6. The Southern Pacific, 1901-1985 

    E-Print Network [OSTI]

    Hofsommer, Don L.

    2008-10-21

    158 Preface xiii 12. The St. Louis Southwestern Railway 177 List of Acronyms and Shortened Names xvii 13. Its Finest Hour 190 CHAPTER 14. Into a Bright Future 208 1. Promontory Prelude 3 15. The Russell Years 225 2. Enter Edward Henry Harriman 9... of the Cotton Belt Route 180 St. Louis Southwestern Railway 181 Topographical map of Southern Pacific 212 Cotton Belt Route 228 Palmdale-Colton Cut-Off 259 Black Mesa Pipeline 261 Alton & Southern 265 Route structure of the Chicago, Rock Island...

  7. Pacific Northwest Smart Grid Demonstration Project

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantityBonneville Power Administration wouldMass mapSpeeding access| Department ofStephen P riceawardsPROCESSINGadVancingPacificPNWSGDP

  8. Meridional Eddy Heat Flux Density: Direct observations of q in the ocean are

    E-Print Network [OSTI]

    Rhode Island, University of

    Meridional Eddy Heat Flux Density: ·Direct observations of q in the ocean are sparse and exhibit large spatio-temporal variability. ·Differential heating of the globe causes a net transport of heat (Qtot) poleward by the ocean and atmosphere. ·Models predict at 36oN in the Pacific that total heat

  9. Role of the ENSOIndian Ocean coupling on ENSO variability in a coupled GCM

    E-Print Network [OSTI]

    Li, Tim

    the key to the rapid transition to an opposite phase. This remote impact of the Indian Ocean SSTanomalyis Nino/La Nina. Without the involvement of the Indian Ocean, the phase transition is much slower linked to the change of zonal wind stress in the western Pacific, which leads to a rapid demise of El

  10. JOUtNALOFGEOPHYSICALRESEARCH VOLUME55, NO.9 SEPTEMBER1950 Natural Radiocarbon in the Atlantic Ocean I

    E-Print Network [OSTI]

    Ocean I WALLACES.BROECKER,ROBERTGERARD,MAURICEEw·, ANDBRUCEC. I-IEEZEN Lamont Geological Observatory may well represent a wedge of young water penetrating the older North Atlantic deep water. Bottom of water along the surface of the Atlantic Ocean,with a return flow at depth. The Atlantic and Pacific

  11. How is the ocean filled? Geoffrey Gebbie1

    E-Print Network [OSTI]

    Huybers, Peter

    hydrographic property to distinguish between North Atlantic Deep Water and Ant- arctic Bottom Water, finding of the deep Pacific than North Atlantic Deep Water. Another answer might be obtained if more water masses were heat, freshwater, and gases with the atmosphere, but once water sinks into the ocean interior

  12. Predictability and Diagnosis of Low-Frequency Climate Processes in the Pacific

    SciTech Connect (OSTI)

    Dr. Arthur J. Miller

    2008-10-15

    Predicting the climate for the coming decades requires understanding both natural and anthropogenically forced climate variability. This variability is important because it has major societal impacts, for example by causing floods or droughts on land or altering fishery stocks in the ocean. Our results fall broadly into three topics: evaluating global climate model predictions; regional impacts of climate changes over western North America; and regional impacts of climate changes over the eastern North Pacific Ocean.

  13. Tapping into Wave and Tidal Ocean Power: 15% Water Power by 2030...

    Broader source: Energy.gov (indexed) [DOE]

    Office What are the key documents? Mapping and Assessment of the United States Ocean Wave Energy Resource pdf here Assessment of Energy Production Potential from Tidal Streams...

  14. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 92, NO. C13, PAGES 14,648-14,662, DECEMBER 15, 1987 On the Parameterization of Irradiance for Open Ocean

    E-Print Network [OSTI]

    Siegel, David A.

    On the Parameterization of Irradiance for Open Ocean Photoprocesses DAVID A. SIEGEL AND T. D. DICKEY Ocean Physics Group of downwelling spectral irradiance were made during the fall of 1982 in the North Pacific Ocean (near 33øN, 142øW). These data are used to produce vertical profiles of downwelling irradiance for visible energy (400-700 nm

  15. Relative Role of Dynamic and Thermodynamic Processes in the Development of the Indian Ocean Dipole: An OGCM Diagnosis

    E-Print Network [OSTI]

    Li, Tim

    in 1997 across the Indo-Pacific Ocean. In the tropical Pacific the largest El Nino in the last 100 years dipole events in the tropical IO, many of which coexisted with El Ninos (Reverdin et al. 1986, Hastenrath et al. 1993, Reason et al. 2000). In fact, the temporal correlation between the El Nino and IO dipole

  16. Eolian inputs of lead to the North Pacific

    SciTech Connect (OSTI)

    Jones, C.E.; Halliday, A.N.; Rea, D.K.; Owen, R.M.

    2000-04-01

    The authors evaluate the importance of natural eolian Pb to the dissolved oceanic Pb budget by measuring the isotopic composition of Pb in 35 Holocene and late Quaternary sediment samples from the North Pacific and in 10 samples of Chinese loess. When the Pacific is divided into sediments provinces based on published {var_epsilon}{sub Nd} and sedimentological data, Pb from the central North Pacific tends to be the most radiogenic and homogeneous due to the dominance of eolian Chinese loess. Lead from the marginal North Pacific and the sparsely sampled regions south of 5{degree}N are less radiogenic and more variable owing to hemipelagic inputs from various volcanic arcs and older continental crust located around the Pacific Rim. {sup 208}Pb/{sup 204}Pb ratios provide the most distinctive provenance information due to the relatively high ratios in Chinese loess. The Chinese loess samples come from 3 localities and span up to 2 Myr of time. Acetic-acid leachate, bulk loess, and loess silicate fractions were analyzed separately. Leachate Pb is considerably less radiogenic than silicate Pb. The isotopic composition of the silicate component closely matches the sediment data from the central North Pacific, confirming the dominance of eolian loess in this region. The authors divided up a suite of published hydrogenous Pb-isotope data from the Pacific Ocean according to their locations within the three independently defined sediment provinces. These data define three distinct fields differentiated primarily by their {sup 206}Pb/{sup 204}Pb ratios, which increase going form the Central to Southern to Marginal provinces. This relationship with sediment province strongly suggests that natural eolian and probably hemipelagic inputs significantly impact the seawater Pb budget. Direct support for the dominance of eolian Chinese loess in the central North Pacific dissolved Pb budget comes from the close match between loess leachate Pb and the Central Province hydrogenous Pb data. Eolian inputs are likely to dominate local seawater Pb budgets only where eolian Pb fluxes are high relative to hemipelagic Pb fluxes and where the flux of Pb carried by deep water advection is low.

  17. Microbe-Metazoan interactions at Pacific Ocean methane seeps

    E-Print Network [OSTI]

    Thurber, Andrew R

    2010-01-01

    B) and those present within methane seep Euryarchaea ( PMI,margin: the influence of methane seeps and oxygen minimumisotope signatures and methane use by New Zealand cold seep

  18. Microbe-metazoan interactions at Pacific Ocean methane seeps

    E-Print Network [OSTI]

    Thurber, Andrew Reichmann

    2010-01-01

    B) and those present within methane seep Euryarchaea ( PMI,margin: the influence of methane seeps and oxygen minimumisotope signatures and methane use by New Zealand cold seep

  19. A decade of acoustic thermometry in the North Pacific Ocean

    E-Print Network [OSTI]

    Frandsen, Jannette B.

    central California (1996­ 1999) and north of Kauai (1997­1999, 2002­2006) transmitted to receivers mounted on the bottom at 183 m depth near Kaneohe, Hawaii, to transmit to bottom-mounted receivers 2000

  20. Subsurface ocean argon disequilibrium reveals the equatorial Pacific shadow zone

    E-Print Network [OSTI]

    David Archer,1 Steven Emerson,2 Charles Stump,2 and Cara Henning3 Received 18 May 2006; revised 27 July with theoretical and model predictions. Citation: Gehrie, E., D. Archer, S. Emerson, C. Stump, and C. Henning (2006 to pathway. Walin [1982], Speer [1997], and Nurser et al. [1999] reason that the production of thermocline

  1. Eastern Equatorial Pacific Ocean Sedimentation: Investigating Constant Flux Proxies 

    E-Print Network [OSTI]

    Singh, Ajay 1980-

    2012-12-03

    of dissolved 230Th concentrations (7.9-16.5 fg/kg) than that within Panama Basin waters (5.7-7.1 fg/kg). There is a progressive decrease, suggesting advection, in average dissolved deep-water (>1000 m) 230Th concentrations from the southernmost sites...

  2. Radiocarbon in dissolved organic carbon of the South Pacific Ocean

    E-Print Network [OSTI]

    Druffel, ERM; Griffin, S

    2015-01-01

    G. Ostlund (1983), Abyssal water C distribution and the agenorthward transport of deep waters, indicating that the deepof Lower Circumpolar Deep Water. This presents a conundrum

  3. Microbe-metazoan interactions at Pacific Ocean methane seeps

    E-Print Network [OSTI]

    Thurber, Andrew Reichmann

    2010-01-01

    lipid biomarkers for microbes with chemoautotrophicOF CALIFORNIA, SAN DIEGO Microbe-Metazoan Interactions atxiv xvii xviii Chapter 3. Microbes, Macrofauna, and Methane:

  4. Microbe-Metazoan interactions at Pacific Ocean methane seeps

    E-Print Network [OSTI]

    Thurber, Andrew R

    2010-01-01

    lipid biomarkers for microbes with chemoautotrophicOF CALIFORNIA, SAN DIEGO Microbe-Metazoan Interactions atxiv xvii xviii Chapter 3. Microbes, Macrofauna, and Methane:

  5. Ocean dynamics and thermodynamics in the tropical Indo- Pacific region

    E-Print Network [OSTI]

    Drushka, Kyla

    2011-01-01

    an effective tsunami warning system for this region.to put an effective tsunami warning system in place. The

  6. Microbe-metazoan interactions at Pacific Ocean methane seeps

    E-Print Network [OSTI]

    Thurber, Andrew Reichmann

    2010-01-01

    2002; Levin et al. 2003; Sommer et al. 2010) whereas clam2001; Levin et al. 2003; Sommer et al. 2006) and frenulaterates (Sommer et al. 2009). Comparable

  7. Microbe-Metazoan interactions at Pacific Ocean methane seeps

    E-Print Network [OSTI]

    Thurber, Andrew R

    2010-01-01

    2002; Levin et al. 2003; Sommer et al. 2010) whereas clam2001; Levin et al. 2003; Sommer et al. 2006) and frenulaterates (Sommer et al. 2009). Comparable

  8. Ocean dynamics and thermodynamics in the tropical Indo- Pacific region

    E-Print Network [OSTI]

    Drushka, Kyla

    2011-01-01

    as the Indonesian Throughflow. Wave energy at a variety ofexamine the properties of wave energy propagating into theto show that intraseasonal wave energy is also effectively

  9. Subtropical ocean ecosystem structure changes forced by North Pacific

    E-Print Network [OSTI]

    Xiu, Peng

    in microalgae, cyano- bacteria and modeled and measured zooplankton biomass were also observed during. While interann- ual trends in mesozooplankton biomass and phyto- plankton pigments have been reported

  10. Ocean dynamics and thermodynamics in the tropical Indo- Pacific region

    E-Print Network [OSTI]

    Drushka, Kyla

    2011-01-01

    compared the spectral energy east and west of Lombok Strait.wave energy bypassed Lombok Strait and continued east alongpropagate east- ward from Lombok to Ombai. Because energy is

  11. Ocean dynamics and thermodynamics in the tropical Indo- Pacific region

    E-Print Network [OSTI]

    Drushka, Kyla

    2011-01-01

    as a proxy for Kelvin wave energy, and comparing the rms SLAas the Indonesian Throughflow. Wave energy at a variety ofexamine the properties of wave energy propagating into the

  12. ARM - Lesson Plans: Temperature of the Pacific Ocean

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantity ofkandz-cm11 Comments?govInstrumentsnoaacrnBarrow, Alaska Outreach Home Room News PublicationsClimatePast

  13. Regional Summary Pacific Region Management Context

    E-Print Network [OSTI]

    Pacific Rim nations. As such, the management of the HMS fisheries s coordinated by the Pacific FisheryRegional Summary Pacific Region Management Context The Pacific Region includes California, Oregon, and Washington. Federal fisheries in this region are managed by the Pacific Fishery Management Council (PFMC

  14. 21st century change in ocean response to climate forcing

    E-Print Network [OSTI]

    Mar?elja, Stjepan

    2015-01-01

    Modeling globally averaged information on climate forcing from the land surface temperature data, the sea surface temperatures (SST) and the empirically determined relationship between the changes in SST and the turbulent diffusion of heat into the upper ocean demonstrates a consistent link. The modeling is accurate throughout the 20th century despite the different phases of the Interdecadal Pacific Oscillation (IPO) or the strong divergence between land and ocean surface warming. It only fails during the last 15 years when SST drops well below the trend. The finding reinforces the view that slower global warming over the previous 15 years is not a caused by a negative phase of the IPO or by the variations in the upper ocean (top 700 m) warming but results from a change in the ocean behavior leading to increased heat transfer into the deeper ocean.

  15. Deep-tow study of magnetic anomalies in the Pacific Jurassic Quiet Zone 

    E-Print Network [OSTI]

    Tominaga, Masako

    2006-10-30

    The Jurassic Quiet Zone (JQZ) is a region of low amplitude, difficult-to-correlate magnetic anomalies located over Jurassic oceanic crust. We collected 1200 km of new deep-tow magnetic anomaly profiles over the Pacific JQZ that complement 2 deep...

  16. The North Pacific Acoustic Laboratory deep-water acoustic propagation experiments in the Philippine Sea

    E-Print Network [OSTI]

    Frandsen, Jannette B.

    The North Pacific Acoustic Laboratory deep-water acoustic propagation experiments in the Philippine in the Philippine Sea during 2009­2011 investigated deep-water acoustic propagation and ambient noise of spanning the water column in the deep ocean. The acoustic transmissions and ambient noise were also

  17. Increased reservoir ages and poorly ventilated deep waters inferred in the glacial Eastern Equatorial Pacific

    E-Print Network [OSTI]

    Fuente, Maria de la; Skinner, Luke; Calvo, Eva; Pelejero, Carles; Cacho, Isabel

    2015-01-01

    % with% other% B@P% records% from% the% northern@% and% southern% high% latitude% Pacific% Ocean% (SWP19,21;% SEP24;% NEP22).% All% of% these% studies%indicate%slightly%higher%B@P%age%offsets%during%the%last%glacial%period%(?200@600%yr...

  18. Micro-phytoplankton biomass of the equatorial Pacific in spring 1992 

    E-Print Network [OSTI]

    Liu, Duan

    1995-01-01

    Along one transect in the eastern equatorial Pacific Ocean the micro-phytoplankton (>15 gm in one dimension) biomass in the upper 200 in was examined. The samples were taken during the most recent El Nifio event and examined in the light microscope...

  19. Size-specific opal-bound nitrogen isotope measurements in North Pacific sediments

    E-Print Network [OSTI]

    Gilli, Adrian

    Size-specific opal-bound nitrogen isotope measurements in North Pacific sediments Anja S. Studer a composition of diatom opal (d15 Ndb) is a valuable recorder of nitrate utilization in the polar surface oceans the measurement of the biogenic opal fraction up to 150 lm in size, which should represent the bulk

  20. New Cities of the Pacific Rim

    E-Print Network [OSTI]

    Edward J. Blakely; Robert J. Stimson

    1992-01-01

    The future cities on the Pacific Rim." Comparative Urban and43 New Cities of the Pacific Rim Edward J. Blakely and43 New Cities of the Pacific Rim Edward J. Blakely and

  1. PacificSouthwestResearchStationPrograms Pacific Southwest Research Station

    E-Print Network [OSTI]

    PacificSouthwestResearchStationPrograms Pacific Southwest Research Station Publications List Air Pollution and Global Change Impacts on Western Forest Ecosystems Center for Urban Forest Research Chemical branch of the USDA Forest Service in the states of California and Hawaii and the U.S.-affiliat- ed

  2. Location Map

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    Lane, Michael

    2013-06-27

    Map file package containing shaded relief base with Hot Pot project area, major roads, railroads, and rivers. The inset map shows regional Paleozoic structural elements.

  3. Location Map

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    Lane, Michael

    Map file package containing shaded relief base with Hot Pot project area, major roads, railroads, and rivers. The inset map shows regional Paleozoic structural elements.

  4. Pacific rim lures explorationists

    SciTech Connect (OSTI)

    Nation, L.

    1991-09-01

    The Pacific Rim has been far and away the most attractive hunting ground for explorationists in the past year. Observers point to political initiatives coupled with a growing demand as igniting the region's numerous hydrocarbon possibilities. This paper describes some of the new incentives and the resultant exploration results and developments in China, Thailand, Malaysia, Indonesia, and Vietnam. A major sign of the region's political maturity is the willingness for the countries involved to solve the longstanding disputes over the claims in hydrocarbon-prone South China Sea.

  5. Accomplishments and future perspective of coastal ocean observing systems Coastal oceans are the most densely urbanized regions on the

    E-Print Network [OSTI]

    are the most densely urbanized regions on the planet with populations growing at rapid rate. In the near future as communities increasingly rely on the coastal ocean to provide additional sources of energy (wind, waves, oil, our ability to map and forecast the coastal ocean remains low. While certain areas are difficult

  6. Independent Oversight Activity Report, Pacific Northwest National...

    Energy Savers [EERE]

    Activity Report, Pacific Northwest National Laboratory - January 2014 Independent Oversight Activity Report, Pacific Northwest National Laboratory - January 2014 February 2014 PNNL...

  7. Independent Oversight Review, Pacific Northwest National Laboratory...

    Energy Savers [EERE]

    September 2013 Independent Oversight Review, Pacific Northwest National Laboratory - September 2013 September 2013 Review of the Fire Protection Program at Pacific Northwest...

  8. Exploring the Deep... Using ArcMap

    E-Print Network [OSTI]

    Wright, Dawn Jeannine

    started Exploring the Ocean Environment Introduction #12;The ArcMap User Interface Table of Contents off the layers above that layer in the Table of Contents. Table of Contents A list of data frames of the current map file. Coordinates Displays the coordinates, in the currently-selected units, of the cursor

  9. PACIFIC SOUTHWEST Forest and Range

    E-Print Network [OSTI]

    PACIFIC SOUTHWEST Forest and Range Experiment Station Ash Leachate Can Reduce Surface Erosion leachate can reduce surface erosion. Res. Note PSW-342, 4 p., illus. Pacific Southwest Forest and Range Exp from north- western California, ash leachate flocculated the clay frac- tions. As a result, the soil

  10. Pacific Northwest Government Contracting Conference

    Broader source: Energy.gov [DOE]

    The Government Contract Assistance Program (GCAP) and Pacific Northwest Defense Coalition (PNDC) cordially invite you to attend our annual Pacific Northwest Government Contracting Conference. The 2015 conference offers a full day of robust and informative training, coupled with networking opportunities. Attendees will learn from seasoned professionals and receive training specifically tailored to companies pursuing the government marketplace.

  11. FOR ADDITIONAL INFORMATION on scientific ocean drilling,please contact Integrated Ocean Drilling Program,Texas A&M University,1000 Discovery Drive,

    E-Print Network [OSTI]

    FOR ADDITIONAL INFORMATION on scientific ocean drilling,please contact Integrated Ocean Drilling.E-mail:information@iodp.tamu.edu; Web:www.iodp-usio.org;Telephone:(979) 845-2673. Design of this map was supported by the Ocean Drilling in this publication do not reflect the views of NSF or Texas A&M University. Deep Sea Drilling Project Legs 1­96,Ocean

  12. GFD-2 OC-513 Spring 2013 P.B. Rhines MWF 10.30-11.20 Ocean Teaching Building 205

    E-Print Network [OSTI]

    => potential vorticity thermal wind · rotation and stratification: the layered, stiffened ocean fluid · Ekman: wind-stress and buoyancy flux · stratification and the `quiet' interior water column · mapping

  13. APRU: Association of Pacific Rim Universities

    E-Print Network [OSTI]

    Takada, Shoji

    No. 549 KYOT O UNIVER SITY FO UN D E D #12;APRU: Association of Pacific Rim Universities APRU APRU Downturn Environment and Development: Scien- tific, Social and Technological Challenges for the Pacific Rim for the Next Century in the Pacific Rim Global Pressures, Local Impacts: Challenge for the Pacific Rim APEC

  14. Pacific Cooperative Studies Unit/Department of Botany, University of Hawai`i Manoa, 3190 Maile Way, St John 410, Honolulu, HI 96822 USA. Email: dduffy@hawaii.edu

    E-Print Network [OSTI]

    Duffy, David Cameron

    ). Cumulatively, Oceania generates less than .01% of world CO2 emissions (Boden et al. 2008). Consequently, the Pacific island states cannot change the trajectory of increasing atmospheric and oceanic CO2. Perhaps the world and Oceania forever. In this paper, Oceania includes the Pacific islands of Micronesia, Melanesia

  15. Migratory shearwaters integrate oceanic resources across the Pacific Ocean in an endless summer

    E-Print Network [OSTI]

    2006-01-01

    signal in primary production with the shearwaters’ migrationonset of migration coincides with the period when primarythe postbreeding migration. Vertically-integrated primary

  16. Science Potential of a Deep Ocean Antineutrino Observatory

    E-Print Network [OSTI]

    Steve Dye

    2006-12-15

    This paper presents science potential of a deep ocean antineutrino observatory under development at Hawaii. The observatory design allows for relocation from one site to another. Positioning the observatory some 60 km distant from a nuclear reactor complex enables precision measurement of neutrino mixing parameters, leading to a determination of neutrino mass hierarchy. At a mid-Pacific location the observatory measures the flux and ratio of uranium and thorium decay neutrinos from earth's mantle and performs a sensitive search for a hypothetical natural fission reactor in earth's core. A subsequent deployment at another mid-ocean location would test lateral heterogeneity of uranium and thorium in earth's mantle.

  17. Ocean Carbon Cycle Data from the Joint Global Ocean Flux Study (JGOFS)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    The U.S. JGOFS program, a component of the U.S Global Change Research Program, grew out of the recommendations of a National Academy of Sciences workshop in 1984. An ambitious goal was set to understand the controls on the concentrations and fluxes of carbon and associated nutrients in the ocean. A new field of ocean biogeochemistry emerged with an emphasis on quality measurements of carbon system parameters and interdisciplinary field studies of the biological, chemical and physical process which control the ocean carbon cycle. U.S. JGOFS, ended in 2005 with the conclusion of the Synthesis and Modeling Project (SMP). Data are available throughout the U.S. JGOFS web site at http://usjgofs.whoi.edu/ and from the U.S. JGOFS Data System at http://usjgofs.whoi.edu/jg/dir/jgofs/. Major named segments of the project are: Bermuda Atlantic Time Series (BATS) Study, Hawaii Ocean Time-series (HOT) Study, Equatorial Pacific Process Study, North Atlantic Bloom Experiment (1989), Arabian Sea Process Study, and the Southern Ocean Process Study.

  18. Ocean Thermal Energy Conversion Basics

    Broader source: Energy.gov [DOE]

    A process called ocean thermal energy conversion (OTEC) uses the heat energy stored in the Earth's oceans to generate electricity.

  19. Pacific Northwest National Laboratory,

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantityBonneville Power Administration wouldMass mapSpeeding access| Department ofStephen P riceawardsPROCESSINGadVancing frontiers in

  20. Climate effects on future runoff regimes of Pacific mountain tributaries

    SciTech Connect (OSTI)

    Rango, A.; Roberts, R. [Agricultural Research Service, Beltsville, MD (United States). Hydrology Lab.; Martinec, J.

    1995-12-31

    Because most Pacific mountain tributaries are situated in the Northern hemisphere, the runoff regime is characterized by high river flows in April-September and low river flows in October--March. With regard to global warming, a partial shift of inflows into the Pacific Ocean from the summer to the winter has to be expected. For quantitative evaluations, the SRM snowmelt runoff model is applied in several basins in the Pacific rim, ranging from 57{degree} North (west coast of Canada) to 45{degree} South (east coast of New Zealand). In the Kings River basin of California (4,000 km{sup 2}, 171--4,341 m a.s.l.) with the envisaged rise of temperature, runoff in October--March is significantly increased at the expense of snow accumulation in winter and summer runoff. Also, summer runoff peaks are shifted to earlier dates. Similar redistribution of runoff is evaluated for the Illecillewaet River basin of British Columbia (1,155 km{sup 2}, 509--3,150 m a.s.l.), a tributary to the Columbia River. However, an additional effect is observed: because nearly 10% of the surface is covered with permanent snowfields and glaciers, runoff would be temporarily increased from these frozen reserves. A quantitative analysis reveals that in the Illecillewaet basin, even a moderate increase of precipitation would not offset a gradual disappearance of glaciers due to increased melting.

  1. ASSESSMENT OF THE WIND RESOURCE AT THE GRACE PACIFIC QUARRY SITE IN KAPOLEI, OAHU

    E-Print Network [OSTI]

    Qiu, Bo

    the feasibility of building a wind farm at Grace Pacific Quarry (GPQ) in Kapolei. This location was chosen because wind maps for Oahu suggest that the location of GPQ has a sufficient wind resource for a wind farm. The people who work at First Wind in Hawaii were interviewed, and the wind resource at their wind farms

  2. Volume III, Chapter 3 Pacific Lamprey

    E-Print Network [OSTI]

    Volume III, Chapter 3 Pacific Lamprey #12;TABLE OF CONTENTS 3.0 Pacific Lamprey (Lampetra................................................................................................... 3-9 3.4.3 Water Development ......................................................................... 3-11 3.4.6 Water Quality

  3. ASSOCIATION OF PACIFIC RIM UNIVERSITIES (APRU) Theme: Global Challenges Pacific Perspectives

    E-Print Network [OSTI]

    Pulfrey, David L.

    ASSOCIATION OF PACIFIC RIM UNIVERSITIES (APRU) Theme: Global Challenges ­ Pacific Perspectives Symposium: APRU Responses to Asia-Pacific Issues Stephen J. Toope, UBC ­ Thursday, July 1, 2010 ASK? These are complex global challenges, yes, but to what extent are they also "Asia-Pacific issues?" Most importantly

  4. MFR PAPER 1160 Assessment of North Pacific

    E-Print Network [OSTI]

    catchers under the jurisdiction of IWC members-in- cluding the "North Pacific Rim" gov- ernments of CanadaMFR PAPER 1160 Assessment of North Pacific Stocks of Whales management of these valuable re- sources. The following report reviews the status of whales and whaling in the north Pacific and summarizes

  5. Climate Change and Pacific Rim Indigenous Nations

    E-Print Network [OSTI]

    Climate Change and Pacific Rim Indigenous Nations BByy AAllaann PPaarrkkeerr,, ZZoollttáánn) 867-6553 E-mail: parkeral@evergreen.edu Web: www.evergreen.edu/nwindian Climate Change and Pacific Rim and drought pat- terns. South Pacific Indigenous peo- ples are finding their islands inundated by rising sea

  6. Agricultural Opportunities in the Pacific Rim

    E-Print Network [OSTI]

    Todd, Brian

    Agricultural Opportunities in the Pacific Rim American Society of Farm Managers and Rural and objectives · Objective: Better understand how agricultural export opportunities in the Pacific Rim and Mexico) are top export destinations and they count as Pacific Rim · Of course, we also import from Canada

  7. Earth MattErsNewsletter of UBC Earth, Ocean and atmospheric sciences Vol. 1 2014

    E-Print Network [OSTI]

    Earth MattErsNewsletter of UBC Earth, Ocean and atmospheric sciences Vol. 1 2014 8 News Transforming undergraduate education, reopening of the Pacific Museum of Earth, and more 18 New Faculty Three on their latest investigations #12;PhotobyKirstenHodge ii EarthMatters 2014 iii Contents iii From the Editor iv

  8. Basin-Wavelength Equatorial Deep Jet Signals Across Three Oceans1 Madeleine K. Youngs2

    E-Print Network [OSTI]

    Johnson, Gregory C.

    of intermediate and deep water masses in the Atlantic. Brandt et al. (2011, 2012) argue38 that as wellBasin-Wavelength Equatorial Deep Jet Signals Across Three Oceans1 Madeleine K. Youngs2 NOAA/Pacific Marine Environmental Laboratory, Seattle WA and Environmental Science and Engineering, California

  9. OCEAN MODEL SIMULATIONS OF A GAP WIND EVENT IN THE GULF OF TEHUANTEPEC

    E-Print Network [OSTI]

    Schultz, David

    winds", are generated as cold air masses surge southward across the Gulf of Mexico and are forced14B.6 OCEAN MODEL SIMULATIONS OF A GAP WIND EVENT IN THE GULF OF TEHUANTEPEC Jon M. Schrage1. INTRODUCTION Off the Pacific coast of southern Mexico, in the Gulf of Tehuantepec, strong northerly winds often

  10. Role of Indian Ocean warming in the development of Philippine Sea anticyclone during ENSO

    E-Print Network [OSTI]

    Watanabe, Masahiro

    Role of Indian Ocean warming in the development of Philippine Sea anticyclone during ENSO Masahiro] The anomalous, low-level anticyclone near the Philippines and suppressed convection over the western Pacific convection over the maritime continent generates the Philippine Sea anticyclone. From a series of the moist

  11. Temporal Data Mining for the Discovery and Analysis of Ocean Climate Indices*

    E-Print Network [OSTI]

    Kumar, Vipin

    , El Nino, the anomalous warming of the eastern tropical region of the Pacific, has been linked America [Tay98]. For this paper, we will be concerned with teleconnections, such as El Nino, that involve of the Earth's oceans. For example, the Southern Oscillation Index (SOI) is an OCI that is associated with El

  12. INTEGRATED OCEAN DRILLING PROGRAM 2011 OCEAN DRILLING CITATION REPORT

    E-Print Network [OSTI]

    INTEGRATED OCEAN DRILLING PROGRAM 2011 OCEAN DRILLING CITATION REPORT covering citations related to the Deep Sea Drilling Project, Ocean Drilling Program, and Integrated Ocean Drilling Program from Geo Drilling Program Publication Services September 2011 #12;OVERVIEW OF THE OCEAN DRILLING CITATION DATABASE

  13. CoastWatch/OceanWatch Proving Ground: VIIRS Ocean Color

    E-Print Network [OSTI]

    ;VIIRS Operational Ocean Color User: NWS/EMC · Phytoplankton alter the penetration of solar radiationCoastWatch/OceanWatch Proving Ground: VIIRS Ocean Color User Engagement, Quality Assessment Science Seminar #12;Outline Overview of VIIRS Ocean Color Proving Ground (Hughes) VIIRS Ocean Color

  14. PACIFIC SOUTHWEST Forest and Range

    E-Print Network [OSTI]

    of forest stands is valuable for studies of the physical environment. Energy balance research centers on howPACIFIC SOUTHWEST Forest and Range Experiment Station FOREST SERVICE U.S. DEPARTMENT in relation to climatic and stand variables USDA FOREST SERVICE RESEARCH PAPER PSW- 71 /1971 #12;CONTENTS

  15. PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER

    E-Print Network [OSTI]

    Baker, Jack W.

    PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER Vector-Valued Ground Motion Intensity Measures of the intensity measures is also shown to be useful for characterizing the effect of near-fault ground motions/08 OCTOBER 2006 #12;Vector-Valued Ground Motion Intensity Measures for Probabilistic Seismic Demand Analysis

  16. Pacific Northwest Solar Radiation Data

    E-Print Network [OSTI]

    Oregon, University of

    Pacific Northwest Solar Radiation Data UO SOLAR MONITORING LAB Physics Department -- Solar Energy Center 1274 University of Oregon Eugene, Oregon 97403-1274 April 1, 1999 #12;Hourly solar radiation data can be obtained from the University of Oregon Solar Moni- toring Laboratory after obtaining permission

  17. Ocean Energy Technology Overview

    SciTech Connect (OSTI)

    none,

    2009-08-05

    Introduction to and overview of ocean renewable energy resources and technologies prepared for the U.S. Department of Energy Federal Energy management Program.

  18. Mapping and Exploring the "Hidden Oregon"

    E-Print Network [OSTI]

    Wright, Dawn Jeannine

    and Space Museum #12;Images courtesy of the National Air and Space Museum #12;#12;#12;#12;#12;Goldfinger et, recreation Oil Spill Response, TrackingWave Energy Navigation Products, Services Maps and Visualizations Port Statement is ... Part of governor's public position on ocean stewardship A suggested process ... (communal

  19. Ocean General Circulation Models

    SciTech Connect (OSTI)

    Yoon, Jin-Ho; Ma, Po-Lun

    2012-09-30

    1. Definition of Subject The purpose of this text is to provide an introduction to aspects of oceanic general circulation models (OGCMs), an important component of Climate System or Earth System Model (ESM). The role of the ocean in ESMs is described in Chapter XX (EDITOR: PLEASE FIND THE COUPLED CLIMATE or EARTH SYSTEM MODELING CHAPTERS). The emerging need for understanding the Earth’s climate system and especially projecting its future evolution has encouraged scientists to explore the dynamical, physical, and biogeochemical processes in the ocean. Understanding the role of these processes in the climate system is an interesting and challenging scientific subject. For example, a research question how much extra heat or CO2 generated by anthropogenic activities can be stored in the deep ocean is not only scientifically interesting but also important in projecting future climate of the earth. Thus, OGCMs have been developed and applied to investigate the various oceanic processes and their role in the climate system.

  20. Oceanic Trace Gases Numeric Data Packages from the Carbon Dioxide Information Analysis Center (CDIAC)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    CDIAC products include numeric data packages, publications, trend data, atlases, models, etc. and can be searched for by subject area, keywords, authors, product numbers, time periods, collection sites, spatial references, etc. Most data sets or packages, many with numerous data files, are free to download from CDIAC's ftp area. CDIAC lists the following numeric data packages under the broad heading of Oceanic Trace Gases: Carbon Dioxide, Hydrographic, and Chemical Data Obtained during the R/V Ronald H. Brown Repeat Hydrography Cruise in the Atlantic Ocean: CLIVAR CO2 Section A16S_2005 ( 01/11/05 - 022405) • Determination of Carbon Dioxide, Hydrographic, and Chemical Parameters during the R/V Nathaniel B. Palmer Cruise in the Southern Indian Ocean (WOCE Section S04I, 050396 - 070496) • Inorganic Carbon, Nutrient, and Oxygen Data from the R/V Ronald H. Brown Repeat Hydrography Cruise in the Atlantic Ocean: CLIVAR CO2 Section A16N_2003a (060403 – 081103) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Maurice Ewing Cruise in the Atlantic Ocean (WOCE Section A17, 010494 - 032194) • Global Ocean Data Analysis Project GLODAP: Results and Data • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Knorr Cruises in the North Atlantic Ocean on WOCE Sections AR24 (1102 – 120596) and A24, A20, and A22 (053097 – 090397) • Carbon Dioxide, Hydrographic and Chemical Data Obtained During the Nine R/V Knorr Cruises Comprising the Indian Ocean CO2 Survey (WOCE Sections I8SI9S, I9N, I8NI5E, I3, I5WI4, I7N, I1, I10, and I2; 120 194 – 012296) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Meteor Cruise 28/1 in the South Atlantic Ocean (WOCE Section A8, 032994 - 051294) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Knorr Cruise 138-3, -4, and -5 in the South Pacific Ocean (WOCE Sections P6E, P6C, and P6W, 050292 - 073092) • Global Distribution of Total Inorganic Carbon and Total Alkalinity below the deepest winter mixed layer depths • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V John V. Vickers Cruise in the Pacific Ocean (WOCE Section P13, NOAA CGC92 Cruise, 080492 – 102192) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Hesperides Cruise in the Atlantic Ocean (WOCE Section A5, 071492 - 081592) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Thomas G. Thompson Cruise in the Pacific Ocean (WOCE Section P10, 100593 – 111093) • The International Intercomparison Exercise of Underway fCO2 Systems during the R/V Meteor Cruise 36/1 in the North Atlantic Ocean • Carbon Dioxide, Hydrographic, and Chemical Data Obtained during the R/V Meteor Cruise 22/5 in the South Atlantic Ocean (WOCE Section A10, Dec. 1992-Jan, 1993) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained in the South Pacific Ocean (WOCE Sections P16A/P17A, P17E/P19S, and P19C, R/V Knorr , Oct. 1992-April 1993) • Surface Water and Atmospheric Underway Carbon Data Obtained During the World Ocean Circulation Experiment Indian Ocean Survey Cruises (R/V Knorr, Dec. 1994 – Jan, 1996) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Akademik Ioffe Cruise in the South Pacific Ocean (WOCE Section S4P, Feb.-April 1992) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Thomas Washington Cruise TUNES-1 in the Equatorial Pacific Ocean (WOCE section P17C) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Thomas Washington Cruise TUNES-3 in the Equatorial Pacific Ocean (WOCE section P16C) • Carbon-14 Measurements in Surface Water CO2 from the Atlantic, Indian and Pacific Oceans, 1965-1994 • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During R/V Meteor Cruise 18/1 in the North Atlantic Ocean (WOCE Section A1E) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained in the Central South Pacific Ocean (WOCE Sections P17S and P16S) during the TUNES-2 Expedition of the R/V Th

  1. Trade war in the Pacific: ASEAN and the Trans-Pacific Partnership https://theconversation.edu.au/trade-war-in-the-pacific-asean-and-the-trans-pacific-partnership-10937[3/12/2012 11:38:09 AM

    E-Print Network [OSTI]

    Botea, Adi

    centred on South-East Asia and a United States-led Pacific Rim. Moreover, it is not clear whetherTrade war in the Pacific: ASEAN and the Trans-Pacific Partnership https://theconversation.edu.au/trade-war-in-the-pacific-asean-and-the-trans-pacific-partnership-10937[3/12/2012 11:38:09 AM] TC Home

  2. Identification of Central-Pacific and Eastern-Pacific types of ENSO in CMIP3 Models

    E-Print Network [OSTI]

    Yu, Jin-Yi; Kim, Seon T.

    2010-01-01

    Cold tongue El Niño and warm pool El Niño, J. Clim. , 22,western?Pacific warm pool, respectively. The identificationthe western Pacific warm pool and others towards the inter-

  3. INV Spring, 2009 1 CANARY ISLANDS (see Atlantic Ocean)

    E-Print Network [OSTI]

    INV Spring, 2009 1 UPD 5/6/15 CANARY ISLANDS (see Atlantic Ocean) 1950 1:100,000 Lanzarote 1950 1:130,000 International travel maps, Canary Islands = Mapas internacionales de viaje, Islas Canarias (bc) - International Nacional 9126/C1/100/1950- 1:100,000 Canary Islands (6 sheets) Mapa Militar: 1 - de la Isla de Hierro 2

  4. Independent Oversight Review, Pacific Northwest National Laboratory...

    Energy Savers [EERE]

    October 2012 Independent Oversight Review, Pacific Northwest National Laboratory - October 2012 October 2012 Review of the Department of Energy Office of Science Assessment of the...

  5. Pacific Northwest National Laboratory Grounds Maintenance

    SciTech Connect (OSTI)

    2009-08-05

    FEMP Water Efficiency Best Management Practice #4 and #5: Case study overview of the grounds maintenance program for Pacific Northwest National Laboratory.

  6. Pacific Fuel Cell Corporation | Open Energy Information

    Open Energy Info (EERE)

    Fuel Cell Corporation Jump to: navigation, search Name: Pacific Fuel Cell Corporation Address: 26985 Lakeland Blvd. Place: Euclid, Ohio Zip: 44132 Sector: Buildings, Efficiency,...

  7. Evaluate Status of Pacific Lamprey in the Clearwater River and Salmon River Drainages, Idaho, 2009 Technical Report.

    SciTech Connect (OSTI)

    Cochnauer, Tim; Claire, Christopher [Idaho Department of Fish and Game

    2009-05-07

    Pacific lamprey Lampetra tridentata have received little attention in fishery science until recently, even though abundance has declined significantly along with other anadromous fish species in Idaho. Pacific lamprey in Idaho have to navigate over eight lower Snake River and Columbia River hydroelectric facilities for migration downstream as juveniles to the Pacific Ocean and again as adults migrating upstream to their freshwater spawning grounds in Idaho. The number of adult Pacific lamprey annually entering the Snake River basin at Ice Harbor Dam has declined from an average of over 18,000 during 1962-1969 to fewer than 600 during 1998-2006. Based on potential accessible streams and adult escapement over Lower Granite Dam on the lower Snake River, we estimate that no more than 200 Pacific lamprey adult spawners annually utilize the Clearwater River drainage in Idaho for spawning. We utilized electrofishing in 2000-2006 to capture, enumerate, and obtain biological information regarding rearing Pacific lamprey ammocoetes and macropthalmia to determine the distribution and status of the species in the Clearwater River drainage, Idaho. Present distribution in the Clearwater River drainage is limited to the lower sections of the Lochsa and Selway rivers, the Middle Fork Clearwater River, the mainstem Clearwater River, the South Fork Clearwater River, and the lower 7.5 km of the Red River. In 2006, younger age classes were absent from the Red River.

  8. Ocean Energy Resource Basics

    Broader source: Energy.gov [DOE]

    Although the potential for ocean energy technologies is believed to be very large, no comprehensive studies have been conducted to date to determine an accurate resource assessment for the United States.

  9. ENCYCLOPEDIA OCEAN SCIENCES

    E-Print Network [OSTI]

    ENCYCLOPEDIA OF OCEAN SCIENCES Editor-in-Chief JOHN H. STEELE Editors STEVE A. THORPE KARL K in Marine Biology 26: 115-168. Rosland Rand Giske .I (1997) A dynamic model for tbe life history

  10. Although tropical cyclones are still not fully understood, Professor Nick Shay was responsible for uncovering the role of the deep ocean on their possible intensification. Here, he

    E-Print Network [OSTI]

    Miami, University of

    of circulation and available upper ocean heat. The HF radar provides a means of mapping surface currents, winds and waves over the coastal ocean to as far as 200 km offshore. These measurements are useful to improve for uncovering the role of the deep ocean on their possible intensification. Here, he explains how his current

  11. Flexible ocean upwelling pipe

    DOE Patents [OSTI]

    Person, Abraham (Los Alamitos, CA)

    1980-01-01

    In an ocean thermal energy conversion facility, a cold water riser pipe is releasably supported at its upper end by the hull of the floating facility. The pipe is substantially vertical and has its lower end far below the hull above the ocean floor. The pipe is defined essentially entirely of a material which has a modulus of elasticity substantially less than that of steel, e.g., high density polyethylene, so that the pipe is flexible and compliant to rather than resistant to applied bending moments. The position of the lower end of the pipe relative to the hull is stabilized by a weight suspended below the lower end of the pipe on a flexible line. The pipe, apart from the weight, is positively buoyant. If support of the upper end of the pipe is released, the pipe sinks to the ocean floor, but is not damaged as the length of the line between the pipe and the weight is sufficient to allow the buoyant pipe to come to a stop within the line length after the weight contacts the ocean floor, and thereafter to float submerged above the ocean floor while moored to the ocean floor by the weight. The upper end of the pipe, while supported by the hull, communicates to a sump in the hull in which the water level is maintained below the ambient water level. The sump volume is sufficient to keep the pipe full during heaving of the hull, thereby preventing collapse of the pipe.

  12. Pacific Ethanol | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home Page on QA:QA J-E-1 SECTION J APPENDIXsourceII JumpQuarterly Smart GridNorth Carolina: EnergyInc the former Jump to:Pacific

  13. Visualization and analysis of eddies in a global ocean simulation

    SciTech Connect (OSTI)

    Williams, Sean J [Los Alamos National Laboratory; Hecht, Matthew W [Los Alamos National Laboratory; Petersen, Mark [Los Alamos National Laboratory; Strelitz, Richard [Los Alamos National Laboratory; Maltrud, Mathew E [Los Alamos National Laboratory; Ahrens, James P [Los Alamos National Laboratory; Hlawitschka, Mario [UC DAVIS; Hamann, Bernd [UC DAVIS

    2010-10-15

    Eddies at a scale of approximately one hundred kilometers have been shown to be surprisingly important to understanding large-scale transport of heat and nutrients in the ocean. Due to difficulties in observing the ocean directly, the behavior of eddies below the surface is not very well understood. To fill this gap, we employ a high-resolution simulation of the ocean developed at Los Alamos National Laboratory. Using large-scale parallel visualization and analysis tools, we produce three-dimensional images of ocean eddies, and also generate a census of eddy distribution and shape averaged over multiple simulation time steps, resulting in a world map of eddy characteristics. As expected from observational studies, our census reveals a higher concentration of eddies at the mid-latitudes than the equator. Our analysis further shows that mid-latitude eddies are thicker, within a range of 1000-2000m, while equatorial eddies are less than 100m thick.

  14. Role of the upper ocean structure in the response of ENSO-like SST variability to global warming

    E-Print Network [OSTI]

    Noh, Yign

    Role of the upper ocean structure in the response of ENSO-like SST variability to global warming)-like variability to global warming varies comparatively between the two different climate system models, i are reduced in the eastern equatorial Pacific under global warming, which erodes the thermo- cline feedback

  15. Our Ocean Backyard Santa Cruz Sentinel columns by Gary Griggs, Director, Institute of Marine Sciences, UC Santa Cruz.

    E-Print Network [OSTI]

    California at Santa Cruz, University of

    from the meltdown of the 3 reactors at the Fukushima Daiichi Nuclear Plant in March 2011 quickly Current as it passes by Japan, whether tsunami debris, glass fishing floats, or radioactive contaminants Nuclear Meltdowns", which provided some interesting perspective on Pacific Ocean radiation. It turns out

  16. Visualising Fe speciation diversity in ocean particulate samples by micro X-ray absorption near-edge spectroscopy

    E-Print Network [OSTI]

    @lbl.gov Environmental context. Iron-bearing particles in the ocean have attracted interest due to the role of iron to something manageable. The Western Subarctic Pacific particles were grouped into four main populations, each into three clusters: (1) Fe3þ -bearing clays þ Fe3þ oxyhydroxides, (2) Fe2þ silicates þ Fe3þ oxyhydroxides

  17. Mapping the Nanoscale Landscape

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Mapping the Nanoscale Landscape Mapping the Nanoscale Landscape Print Wednesday, 27 September 2006 00:00 For the first time, researchers have successfully mapped the chemical...

  18. Now Available: Pacific Northwest Smart Grid Demonstration Project...

    Energy Savers [EERE]

    Now Available: Pacific Northwest Smart Grid Demonstration Project - Technology Performance Report Volume 1 Now Available: Pacific Northwest Smart Grid Demonstration Project -...

  19. Energy, Transportation Ministers from Asia-Pacific Nations Pledge...

    Office of Environmental Management (EM)

    Transportation Ministers from Asia-Pacific Nations Pledge Cooperation on Cleaner, More Energy-Efficient Transportation Energy, Transportation Ministers from Asia-Pacific Nations...

  20. SeaPower Pacific subsidiary of Renewable Energy Holdings Plc...

    Open Energy Info (EERE)

    SeaPower Pacific subsidiary of Renewable Energy Holdings Plc Carnegie Corporation Ltd Jump to: navigation, search Name: SeaPower Pacific subsidiary of Renewable Energy Holdings Plc...

  1. Preliminary Notice of Violation, Pacific Data Electric, Inc....

    Office of Environmental Management (EM)

    Pacific Data Electric, Inc. - February 12, 2015 February 12, 2015 Worker Safety and Health Enforcement Preliminary Notice of Violation issued to Pacific Data Electric, Inc. On...

  2. Department of Energy Cites the University of California and Pacific...

    Office of Environmental Management (EM)

    the University of California and Pacific Data Electric, Inc., for Worker Safety and Health Program Violations Department of Energy Cites the University of California and Pacific...

  3. NORTHEAST PACIFIC ALBACORE OCEANOGRAPHY SURVEY, 1961

    E-Print Network [OSTI]

    444 NORTHEAST PACIFIC ALBACORE OCEANOGRAPHY SURVEY, 1961 by R. W. Owen, Jr. SPECIAL SCIENTIFIC OCEANOGRAPHY SURVEY, 1961 by R, W. Owen, Jr. United States Fish and Wildlife Service Special Scientific Report PACIFIC ALBACORE OCEANOGRAPHY SURVEY, 1961 by R. W. Owen, Jr. Fishery Biologist Research Bureau

  4. NORTH PACIFIC OCEANOGRAPHY, FEBRUARY-APRIL 1962

    E-Print Network [OSTI]

    477: NORTH PACIFIC OCEANOGRAPHY, FEBRUARY- APRIL 1962 by Felix Favorite, Betty-Ann Morse, Alan H'auUke, Commissioner Bureau of Commep.cial FlSHERif;s, Donald L. McKernan, Director NORTH PACIFIC OCEANOGRAPHY OCEANOGRAPHY, FEBRUARY - APRIL 1962 by Felix Favorite and Betty-Ann Morse, Oceanographers Alan H. Haselwood

  5. Royal Pacific: Order (2013-SE-33004)

    Broader source: Energy.gov [DOE]

    DOE ordered Royal Pacific, Ltd. to pay a $8,000 civil penalty after finding Royal Pacific had failed to certify that various basic models of medium base compact fluorescent lamps, ceiling fans, ceiling fan light kits, and illuminated exit signs comply with the applicable energy conservation standards.

  6. Pacific and Atlantic herring produce burst pulse

    E-Print Network [OSTI]

    Dill, Lawrence M.

    Pacific and Atlantic herring produce burst pulse sounds Ben Wilson1,2* , Robert S. Batty3 wild-caught herring. Pacific herring pro- duce distinctive bursts of pulses, termed Fast Repetitive Tick (FRT) sounds. These trains of broadband pulses (1.7­22 kHz) lasted between 0.6 s and 7.6 s. Most

  7. Pacific Northwest Power Supply Adequacy Assessment

    E-Print Network [OSTI]

    1 Pacific Northwest Power Supply Adequacy Assessment for 2019 Final Report May 7, 2014 Council Document Number 2014-04 #12;2 Executive Summary The Pacific Northwest's power supply is expected resources: demand-side actions and emergency resources used only during shortages. The assumption about

  8. Demand Response Resources in Pacific Northwest

    E-Print Network [OSTI]

    Demand Response Resources in Pacific Northwest Chuck Goldman Lawrence Berkeley National Laboratory cagoldman@lbl.gov Pacific Northwest Demand Response Project Portland OR May 2, 2007 #12;Overview · Typology Annual Reports ­ Journal articles/Technical reports #12;Demand Response Resources · Incentive

  9. Partnerships in the Pacific Rim

    SciTech Connect (OSTI)

    Wendorf, A.W. [Sargent and Lundy, Chicago, IL (United States). Power Generation Services

    1997-09-01

    Due to the ever-increasing need to use global marketing as a means of gaining new business, Sargent and Lundy, like many of its competitors, has looked to stronger partnering relationships (e.g. alliances, teaming agreements, etc.) to enhance its ability to compete. New power generation plants, often developed, owned and operated by independent power companies in pacific Rim countries is one of the greatest sources of new business for engineering firms prepared to compete in this arena. In general, Sargent and Lundy focuses on three types of partnering relationships developed for international power markets in pacific Rim countries. These three relationships can be summarized as follows: partnering with other US-based organizations; partnering with non-US based organizations located in a country different than that of the intended market; and partnering with organizations located in the same country as the intended market. The features of each of the three partnering relationships discussed here involve considerable business development and logistics considerations and many other details that generally do not affect US-based partnering arrangements focusing on US business. The situation-specific details necessary to develop a successful partnering relationship depend greatly upon the client`s needs as well as the final goals of all companies involved.

  10. Mesoscale coupled ocean-atmosphere interaction

    E-Print Network [OSTI]

    Seo, Hyodae

    2007-01-01

    mesoscale oceanic features are current coarse resolutionmesoscale r current variability associated with oceanic ringthe TIW- currents. These mesoscale oceanic and atmospheric

  11. Mesoscale Coupled Ocean-Atmosphere Interaction

    E-Print Network [OSTI]

    Seo, Hyodae

    2007-01-01

    mesoscale oceanic features are current coarse resolutionmesoscale r current variability associated with oceanic ringthe TIW- currents. These mesoscale oceanic and atmospheric

  12. Ocean Thermal Extractable Energy Visualization: Final Technical...

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Ocean Thermal Extractable Energy Visualization: Final Technical Report Ocean Thermal Extractable Energy Visualization: Final Technical Report Report about the Ocean Thermal...

  13. Tropical Western Pacific site science mission plan. Semiannual project report, January--June 1998

    SciTech Connect (OSTI)

    Ackerman, T.; Mather, J.; Clements, W.; Barnes, F.

    1998-11-01

    The Department of Energy`s Atmospheric Radiation Measurement (ARM) program was created in 1989 as part of the US Global Change Research Program to improve the treatment of atmospheric radiative and cloud processes in computer models used to predict climate change. The overall goal of the ARM program is to develop and test parameterizations of important atmospheric processes, particularly cloud and radiative processes, for use in atmospheric models. This goal is being achieved through a combination of field measurements and modeling studies. Three primary locales were chosen for extensive field measurement facilities. These are the Southern Great Plains (SGP) of the United States, the Tropical Western Pacific (TWP), and the North Slope of Alaska and Adjacent Arctic Ocean (NSA/AAO). This Site Science Mission Plan [RPT(TWP)-010.000] describes the ARM program in the Tropical Western Pacific locale.

  14. Site Map

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantity of NaturalDukeWakefieldSulfateSciTechtail.Theory ofDidDevelopment Top Scientific ImpactTechnologies |Site IndexSite Map

  15. Site Map

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantity ofkandz-cm11 Outreach Home RoomPreservation ofAlbuquerque|Sensitive Species3 Outlook forSimulationsSite Map TUNL pdf's |

  16. 2010 Ecological Survey of the Pacific Northwest National Laboratory Site

    SciTech Connect (OSTI)

    Chamness, Michele A.; Perry, Christopher; Downs, Janelle L.; Powell, Sylvia D.

    2011-02-16

    The U.S. Department of Energy (DOE) Pacific Northwest Site Office (PNSO) oversees and manages the DOE contract for the Pacific Northwest National Laboratory (PNNL), a DOE Office of Science multi-program laboratory located in Richland, Washington. PNSO is responsible for ensuring that all activities conducted on the PNNL Site comply with applicable laws, policies, and DOE orders. The DOE Pacific Northwest Site Office Cultural and Biological Resources Management Plan (DOE/PNSO 2008) addresses the requirement for annual surveys and monitoring for species of concern and to identify and map invasive species. In addition to the requirement for an annual survey, proposed project activities must be reviewed to assess any potential environmental consequences of conducting the project. The assessment process requires a thorough understanding of the resources present, the potential impacts of a proposed action to those resources, and the ultimate consequences of those actions. The PNNL Site is situated on the southeastern corner of the DOE Hanford Site, located at the north end of the city of Richland in south-central Washington. The site is bordered on the east by the Columbia River, on the west by Stevens Drive, and on the north by the Hanford Site 300 Area (Figure 1). The environmental setting of the PNNL Site is described in Larson and Downs (2009). There are currently two facilities on the PNNL Site: the William R. Wiley Environmental Molecular Sciences Laboratory (EMSL), and the recently completed Physical Sciences Facility (PSF). This report describes the results of the annual survey of the biological resources found on the undeveloped portions of the PNNL Site in 2010. A brief description of the methods PNNL ecologists used to conduct the surveys and the results of the surveys are presented. Actions taken to fully delineate noxious weed populations discovered in 2009 and efforts in 2010 to control those weeds also are described. Appendix A provides a list of plant and animal species identified on the PNNL Site.

  17. M.S. Economic Geology, Oregon State University College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR Expected Spring, 2015

    E-Print Network [OSTI]

    Kurapov, Alexander

    EDUCATION M.S. Economic Geology, Oregon State University College of Earth, Ocean. Dilles Relevant Courses Interpretation of Geologic Maps Igneous Petrology Tectonic Geomorphology B.S. Geology, University of Idaho College of Science, Moscow, ID; GPA: 3

  18. Massachusetts Ocean Management Plan (Massachusetts)

    Broader source: Energy.gov [DOE]

    The Massachusetts Ocean Act of 2008 required the state’s Secretary of Energy and Environmental Affairs to develop a comprehensive ocean management plan for the state by the end of 2009. That plan...

  19. Steroid estrogens in ocean sediments 

    E-Print Network [OSTI]

    Braga, O.; Smythe, G.A.; Schäfer, Andrea; Feitz, A.J.

    2005-01-01

    This paper gives results from a study measuring the abundance of steroid hormones in ocean sediments in the proximity of a deep ocean sewage outfall. The outfall is discharge point for an enhanced primary sewage treatment ...

  20. Independent Oversight Inspection, Pacific Northwest National Laboratory- December 2003

    Broader source: Energy.gov [DOE]

    Inspection of Environment, Safety, and Health Management at the Pacific Northwest National Laboratory

  1. Pacific Rim Summit on Industrial Biotechnology & Bioenergy

    Broader source: Energy.gov [DOE]

    The ninth annual Pacific Rim Summit on Industrial Biotechnology and Bioenergy will be held from December 7–9, 2014, in San Diego, California, at the Westin Gaslamp Quarter. Bringing together representatives from various countries all around the Pacific Rim, this event will focus on the growth of the industrial biotechnology and bioenergy sectors in North America and the Asia-Pacific region. Glenn Doyle, BETO's Deployment & Demonstration Technology Manager, will be moderating and speaking at a session on entitled "Utilizing Strategic Partnerships to Grow Your Business" on December 9.

  2. Mapping and Assessment of the United States Ocean Wave Energy...

    Open Energy Info (EERE)

    Download Full Report URL: http:en.openei.orgdatasetsdataset6b40f428-2af0-40b3-8a53-0c32c7e35973resource9bfc4b34-78a1-4da9-8928-48a1f72ee8e8downloadmappingandassessmentofth...

  3. Mapping and Assessment of the United States Ocean Wave Energy...

    Open Energy Info (EERE)

    have recovered by 5 cm when DSPR 30, but only by 1-2 cm when DSPR 10. Source: Smith et al. (2007). ... 2-14 Figure 2-9 Wave height reduction for a 90%...

  4. Mapping and Assessment of the United States Ocean Wave Energy...

    Open Energy Info (EERE)

    Source http:my.epri.comportalserver.pt?Productid000000000001024637 Author EPRI Catalog OpenEI Origination Date 2011-12-05T00:00:00 Required Software Sectors Water...

  5. Alien Maps of an Ocean-Bearing World

    E-Print Network [OSTI]

    Cowan, Nicolas B.

    When Earth-mass extrasolar planets first become detectable, one challenge will be to determine which of these worlds harbor liquid water, a widely used criterion for habitability. Some of the first observations of these ...

  6. Ocean Engineering Development Team

    E-Print Network [OSTI]

    Wood, Stephen L.

    the same conditions). 3) To demonstrate a working knowledge of fluid mechanics, naval architecture: Design/Fluid Mechanics Major: Ocean Engineering, Junior Focus: Naval Architecture and High Speed Small vessel under a variety of foil configurations, sea conditions, propulsion states and loads. 2) To perform

  7. Reduced ventilation and enhanced magnitude of the deep Pacific carbon pool during the last glacial period

    E-Print Network [OSTI]

    Skinner, L.; McCave, I. N.; Carter, L.; Fallon, S.; Scrivner, A. E.; Primeau, F.

    2014-12-15

    to mid-depth radiocarbon-age difference over the last 20 kyr. Earth Planet. Sci. Lett. 274, 322–326. onk Ramsey, C., Staff, R.A., Bryant, C.L., Brock, F., Kitagawa, H., van der Plicht, J., Schlolaut, G., Marshall, M.H., Brauer, A., Lamb, H.F., Payne, R... at intermediate water depth in the Pacific Ocean during the last deglaciation. Paleoceanography 24, PA2223. Stuiver, M., Polach, H.A., 1977. Reporting of 14C data. Radiocarbon 19, 355–363. Talley, L.D., Pickard, G.L., Emery, W.J., Swift, J.H., 2011. Descriptive...

  8. Rethinking Tropical Ocean Response to Global Warming: The Enhanced Equatorial Warming*

    E-Print Network [OSTI]

    Wisconsin at Madison, University of

    of tropical Pacific SST to increased atmospheric CO2 concentration is reexamined with a new focus in Fig. 1, which shows the SST trends in response to a 1% transient CO2 in- crease in 14 fully coupled.gov/ipcc/about_ipcc.php), and 1 as an in-house Fast Ocean­Atmosphere Model (FOAM; Jacob 1997). If we define the El Niño

  9. Ocean Circulation Lynne D Talley

    E-Print Network [OSTI]

    Talley, Lynne D.

    to the topography, with low pressure in the center. Ocean currents transport heat from the tropics to the poles have gone to sea. As knowledge about ocean currents and capabilities to observe it below the surfaceOcean Circulation Lynne D Talley Volume 1, The Earth system: physical and chemical dimensions

  10. 6, 51375162, 2006 Oceanic ozone

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    ACPD 6, 5137­5162, 2006 Oceanic ozone deposition velocity C. W. Fairall et al. Title Page Abstract Discussions Water-side turbulence enhancement of ozone deposition to the ocean C. W. Fairall1 , D. Helmig2 , L. Fairall (chris.fairall@noaa.gov) 5137 #12;ACPD 6, 5137­5162, 2006 Oceanic ozone deposition velocity C. W

  11. Strategic Plan National Ocean Service

    E-Print Network [OSTI]

    Strategic Plan of the National Ocean Service 2005-2010 U.S. Department of Commerce National Oceanic Strategic Plan for 2005 to 2010. This Plan heralds a new era for the ocean and coasts as NOS responds these challenges. The NOS Strategic Plan is synchronous with the NOAA Strategic Plan -- one NOAA, one workforce

  12. December 2001 OCEAN DRILLING PROGRAM

    E-Print Network [OSTI]

    December 2001 OCEAN DRILLING PROGRAM LEG 203 SCIENTIFIC PROSPECTUS DRILLING AT THE EQUATORIAL -------------------------------- Dr. Jack Bauldauf Deputy Director of Science Operations Ocean Drilling Program Texas A&M University. Acton Leg Project Manager and Staff Scientist Ocean Drilling Program Texas A&M University 1000 Discovery

  13. February 2002 OCEAN DRILLING PROGRAM

    E-Print Network [OSTI]

    February 2002 OCEAN DRILLING PROGRAM LEG 204 SCIENTIFIC PROSPECTUS DRILLING GAS HYDRATES ON HYDRATE -------------------------------- Dr. Jack Baldauf Deputy Director of Science Operations Ocean Drilling Program Texas A&M University Richter Leg Project Manager and Staff Scientist Ocean Drilling Program Texas A&M University 1000 Discovery

  14. November 2002 OCEAN DRILLING PROGRAM

    E-Print Network [OSTI]

    November 2002 OCEAN DRILLING PROGRAM LEG 208 SCIENTIFIC PROSPECTUS EARLY CENOZOIC EXTREME CLIMATES -------------------------------- Dr. Jack Baldauf Deputy Director of Science Operations Ocean Drilling Program Texas A&M University Leg Project Manager and Staff Scientist Ocean Drilling Program Texas A&M University 1000 Discovery

  15. Engineering by Design Ocean Engineering

    E-Print Network [OSTI]

    Virginia Tech

    Engineering by Design Ocean Engineering Bachelor of Science Degree Virginia Tech For more engineering is a diverse field. At Virginia Tech, the major focus areas are ocean energy systems and ocean in the aerospace and related industries and in the shipbuilding, naval engineering, and ship design fields. Some

  16. Ninth Annual Ocean Renewable Energy Conference

    Broader source: Energy.gov [DOE]

    The future of clean, renewable ocean wave energy will be discussed in depth at the 2014 Ocean Renewable Energy Conference.

  17. Polar Sea Ice Mapping Using SeaWinds Data Hyrum S. Anderson and David G. Long

    E-Print Network [OSTI]

    Long, David G.

    of Bayes detection to produce sea ice extent maps. Statistical models for sea ice and ocean are represented of their independence of solar illumination, their ability to penetrate to ever-present canopy of clouds in the polar of these same measure- ments. The A imagery exhibits good statistical contrast between sea ice and ocean

  18. Miocene-Early Pliocene diatomaceous sedimentation patterns in the Pacific: A response to paleooceanography and paleoclimatic change

    SciTech Connect (OSTI)

    Barron, J.A. )

    1990-05-01

    Biosiliceous sediments greatly expanded their distribution in the North Pacific during the late early to early middle Miocene (18-15 Ma), at least partly due to enhanced basin-basin fractionation of deep waters between the North Atlantic and North Pacific, which began in 17 Ma. Subsequently, in the late middle and late Miocene, diatomaceous sedimentation responded to the following series of successive cooling steps. (1) High-latitude cooling between 14.9 and 12.4 Ma caused an intensification of upwelling in the marginal North Pacific as evidenced by a wider distribution of laminated sediments and a decline in carbonate preservation. (2) Cooling across the middle Miocene-late Miocene boundary (10.3-9.2 Ma and 9.0-8.3 Ma) led to further increases in upwelling and raised biogenic opal accumulation rates in upwelling regions of the eastern equatorial Pacific, California, and Peru. (3) Cooling in the latest Miocene to earliest Pliocene (6.2-4.8 114a) resulted in further regional differentiation of biosiliceous sedimentation patterns in the North Pacific, probably reflecting steeper productivity gradients in upwelling regions. Biogenic opal accumulation rates declined in the eastern equatorial Pacific, but probably increased in coastal upwelling regions off California, Peru, and in the Bering Sea. (4) A decline in diatom sedimentation in waters off southern California during the earliest Pliocene (4.5-4.0) Ma coincided with a period of warmer paleotemperatures and a decline in opal accumulation rates in the equatorial Pacific. A major increase in biosiliceous sedimentation in the Southern ocean occurred at this same time.

  19. Particulate matter in the central subtropical Pacific 

    E-Print Network [OSTI]

    Colgan, Annette Renee

    1995-01-01

    The distribution of particulate matter (PM) in the Central Subtropical Pacific and its relationships with water masses and currents were determined from optical and hydrographic data. Beam attenuation data were collected with a Sea Tech...

  20. Royal Pacific: Proposed Penalty (2013-SE-33004)

    Broader source: Energy.gov [DOE]

    DOE alleged in a Notice of Proposed Civil Penalty that Royal Pacific, Ltd. failed to certify ceiling fans, ceiling fan light kits, medium base compact fluorescent lamps, and illuminated exit signs as compliant with the applicable energy conservation standards.

  1. 1993 Pacific Northwest Loads and Resources Study.

    SciTech Connect (OSTI)

    United States. Bonneville Power Administration.

    1993-12-01

    The Loads and Resources Study is presented in three documents: (1) this summary of Federal system and Pacific Northwest region loads and resources; (2) a technical appendix detailing forecasted Pacific Northwest economic trends and loads, and (3) a technical appendix detailing the loads and resources for each major Pacific Northwest generating utility. In this loads and resources study, resource availability is compared with a range of forecasted electricity consumption. The forecasted future electricity demands -- firm loads -- are subtracted from the projected capability of existing and {open_quotes}contracted for{close_quotes} resources to determine whether Bonneville Power Administration (BPA) and the region will be surplus or deficit. If resources are greater than loads in any particular year or month, there is a surplus of energy and/or capacity, which BPA can sell to increase revenues. Conversely, if firm loads exceed available resources, there is a deficit of energy and/or capacity, and additional conservation, contract purchases, or generating resources will be needed to meet load growth. The Pacific Northwest Loads and Resources Study analyzes the Pacific Northwest`s projected loads and available generating resources in two parts: (1) the loads and resources of the Federal system, for which BPA is the marketing agency; and (2) the larger Pacific Northwest regional power system, which includes loads and resource in addition to the Federal system. The loads and resources analysis in this study simulates the operation of the power system under the Pacific Northwest Coordination Agreement (PNCA) produced by the Pacific Northwest Coordinating Group. This study presents the Federal system and regional analyses for five load forecasts: high, medium-high, medium, medium-low, and low. This analysis projects the yearly average energy consumption and resource availability for Operating Years (OY) 1994--95 through 2003--04.

  2. Geologic Maps Geology 200

    E-Print Network [OSTI]

    Kammer, Thomas

    Geologic Maps Geology 200 Geology for Environmental Scientists #12;Geologic Map of the US #12;Symbols found on geologic maps #12;Horizontal Strata #12;Geologic map of part of the Grand Canyon. Each color represents a different formation. #12;Inclined Strata #12;Dome #12;Geologic map of the Black Hills

  3. TransCom 3 inversion intercomparison: Impact of transport model errors on the interannual variability of regional CO 2 fluxes, 1988-2003

    E-Print Network [OSTI]

    2006-01-01

    East Pacific South Pacific Northern Ocean North AtlanticEast Pacific South Pacific Northern Ocean North Atlanticand South Pacific, and the Northern Ocean) for which there

  4. Mahuzuddin, editors. Conservation of Pacific Sea turtles. University of Hawaii Press, Honolulu, Hawaii, USA.

    E-Print Network [OSTI]

    Gerber, Leah R.

    . Pacific Island microstates: Pawns or players in Pacific Rim diplomacy? Diplomacy and Statecraft 17Mahuzuddin, editors. Conservation of Pacific Sea turtles. University of Hawaii Press, Honolulu

  5. ``Plate-like'' subsidence of the East Pacific RiseSouth Pacific superswell system

    E-Print Network [OSTI]

    Watts, A. B. "Tony"

    ``Plate-like'' subsidence of the East Pacific Rise­­South Pacific superswell system J. K. Hillier significantly, the superswell appears to be part of a large-scale, ``plate-like,'' subsidence that extends to the EPR crest, rather than an isolated shallowing that reverses the subsidence and causes uplift. We

  6. A COMPARISON OF ACOUSTIC THERMOMETRY, XBT, TOPEX, AND HOT OBSERVATIONS OF OCEAN TEMPERATURE IN THE NORTHEAST PACIFIC OCEAN

    E-Print Network [OSTI]

    Dushaw, Brian

    , while the timeseries from a source north of Kauai, Hawaii began in late 1997. As a result of marine between Hawaii and California using the Kauai source with no corresponding variability in the TOPEX data after 24 months of operation in accord with permit requirements. Transmissions from the Kauai source

  7. Iron isotopes in the seawater of the equatorial Pacific Ocean: New constraints for the oceanic iron cycle

    E-Print Network [OSTI]

    Murray, James W.

    only explain a fraction of the last glacial maximum CO2 drawdown (Kohfeld et al., 2005), they confirmed to the CO2 drawdown observed in the last glacial maximum. This hypothesis motivated numerous studies focused are positive (relative to IRMM-14), from +0.01 to +0.58 in the dissolved fraction (DFe) and from -0.02 to +0

  8. “Deep Maps”: A Brief for Digital Palimpsest Mapping Projects (DPMPs, or “Deep Maps”)

    E-Print Network [OSTI]

    Fishkin, Shelley Fisher

    2011-01-01

    DEEP  MAPS”:  A  Brief  for   Digital  Projects   (DPMPs,  or  “Deep  Maps”)   SHELLEY  FISHER  acronym   DPMPs   as   “Deep   Maps. ”   They   would  

  9. OCEAN VOLCANO CAUGHT ON FILM Footage of a volcanic eruption nearly 1,200 metres under the sea was unveiled on 17 December at a meeting of

    E-Print Network [OSTI]

    Rosenberg, Noah

    OCEAN VOLCANO CAUGHT ON FILM Footage of a volcanic eruption nearly 1,200 metres under the sea. The high-definition film of the West Mata volcano in the western Pacific is one of the first times to raise up to US$300 million. Founded in 2005, Solyndra makes thin- film cylindrical modules for use

  10. ON THE INSTABILITY OF TROPICAL WESTERN PACIFIC WARM POOL DURING THE BOREAL WINTER AND SPRING

    SciTech Connect (OSTI)

    BARR-KUMARAKULASINGHE,S.A.

    1998-03-23

    A source of instability in the western Pacific warm pool is shown to be due to sea surface elevation variations caused by changes in the zonal sea-surface temperature (SST) gradient and the changes in the Pacific Ocean basin length in relation to the warm pool latitudinal location. The variation of the sea-surface elevation is measured by using the thermocline depth response calculated from a two-layer ocean. The warm pool is shown to be barely at equilibrium during the boreal late winter and early spring by comparing the measured thermocline at 110{degree}W, 0{degree}E with the calculated thermocline depth. Based on this analysis, a failure or reversal of the climatological zonal winds are apparently not a necessary precursor for the instability of the warm pool and initiation of a warm event. A warm event can be initiated by an increase in the size of the warm pool and/or an increase in zonal SST differences during the boreal/winter spring. This mechanism could be an alternate mechanism for El-Nino Southern Oscillation (ENSO) dynamics to that postulated by Bjeknes (1969).

  11. VOCALS: The VAMOS Ocean-Cloud-Atmosphere-Land Study

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    Wood, Robert [VOCALS-REx PI, University of Washington; Bretherton, Christopher [GEWEX/GCSS Representative, University of Washington; Huebert, Barry [SOLAS Representative, University of Hawaii; Mechoso, Roberto C. [VOCALS Science Working Group Chair, UCLA; Weller, Robert [Woods Hole Oceanographic Institution

    VOCALS (VAMOS* Ocean-Cloud-Atmosphere-Land Study) is an international CLIVAR program the major goal of which is to develop and promote scientific activities leading to improved understanding of the Southeast Pacific (SEP) coupled ocean-atmosphere-land system on diurnal to inter-annual timescales. The principal program objectives are: 1) the improved understanding and regional/global model representation of aerosol indirect effects over the SEP; 2) the elimination of systematic errors in the region of coupled atmospheric-ocean general circulation models, and improved model simulations and predictions of the coupled climate in the SEP and global impacts of the system variability. VOCALS is organized into two tightly coordinated components: 1) a Regional Experiment (VOCALSREx), and 2) a Modeling Program (VOCALS-Mod). Extended observations (e.g. IMET buoy, satellites, EPIC/PACS cruises) will provide important additional contextual datasets that help to link the field and the modeling components. The coordination through VOCALS of observational and modeling efforts (Fig. 3) will accelerate the rate at which field data can be used to improve simulations and predictions of the tropical climate variability [Copied from the Vocals Program Summary of June 2007, available as a link from the VOCALS web at http://www.eol.ucar.edu/projects/vocals/]. The CLIVAR sponsored program to under which VOCALS falls is VAMOS, which stands for Variability of the American Monsoon Systems.

  12. OCEAN THERMAL ENERGY CONVERSION (OTEC) PROGRAMMATIC ENVIRONMENTAL ANALYSIS

    E-Print Network [OSTI]

    Sands, M. D.

    2011-01-01

    310, the Ocean the Ocean Energy Thermal Energy Conversionfor the commercialization of ocean thermal energy conversionOpen cycle ocean thermal energy conversion. A preliminary

  13. Ocean Adventurer ---Overview---

    E-Print Network [OSTI]

    Jaffe, Jules

    background map with the data grid It took a little thinking for me to figure this part out but, the trick. After in-putting your grid of choice, you can use the browser and zoom in on the display. Screen shot Fixes Text boxes in the game can be deleted and/or additional information can be added into it. Not very

  14. Ocean Thermal Extractable Energy Visualization

    SciTech Connect (OSTI)

    Ascari, Matthew

    2012-10-28

    The Ocean Thermal Extractable Energy Visualization (OTEEV) project focuses on assessing the Maximum Practicably Extractable Energy (MPEE) from the world’s ocean thermal resources. MPEE is defined as being sustainable and technically feasible, given today’s state-of-the-art ocean energy technology. Under this project the OTEEV team developed a comprehensive Geospatial Information System (GIS) dataset and software tool, and used the tool to provide a meaningful assessment of MPEE from the global and domestic U.S. ocean thermal resources.

  15. ARM - Oceanic Properties

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantity ofkandz-cm11 Comments?govInstrumentsnoaacrnBarrow, Alaska OutreachCalendar NSA Related Links AntarcticaNews fromOceanic

  16. Ocean | Open Energy Information

    Open Energy Info (EERE)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home Page on QA:QA J-E-1 SECTION J APPENDIX ECoop Inc Jump to:Newberg, Oregon:OGE Energy Resources, IncIncOccidental,OceanLtd

  17. Impacts of ocean albedo alteration on Arctic sea ice restoration and Northern Hemisphere climate

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Cvijanovic, Ivana; Caldeira, Ken; MacMartin, Douglas G.

    2015-04-01

    The Arctic Ocean is expected to transition into a seasonally ice-free state by mid-century, enhancing Arctic warming and leading to substantial ecological and socio-economic challenges across the Arctic region. It has been proposed that artificially increasing high latitude ocean albedo could restore sea ice, but the climate impacts of such a strategy have not been previously explored. Motivated by this, we investigate the impacts of idealized high latitude ocean albedo changes on Arctic sea ice restoration and climate. In our simulated 4xCO? climate, imposing surface albedo alterations over the Arctic Ocean leads to partial sea ice recovery and a modestmore »reduction in Arctic warming. With the most extreme ocean albedo changes, imposed over the area 70°–90°N, September sea ice cover stabilizes at ~40% of its preindustrial value (compared to ~3% without imposed albedo modifications). This is accompanied by an annual mean Arctic surface temperature decrease of ~2 °C but no substantial global mean temperature decrease. Imposed albedo changes and sea ice recovery alter climate outside the Arctic region too, affecting precipitation distribution over parts of the continental United States and Northeastern Pacific. For example, following sea ice recovery, wetter and milder winter conditions are present in the Southwest United States while the East Coast experiences cooling. We conclude that although ocean albedo alteration could lead to some sea ice recovery, it does not appear to be an effective way of offsetting the overall effects of CO? induced global warming.« less

  18. 90E 120 150E 180 150W 120 90 60 30W 0 30E 60 DSDP Legs 196 ( ), ODP Legs 100210 ( ), IODP Expeditions 301352 ( )

    E-Print Network [OSTI]

    GREENLAND EUROPE AFRICA SOUTH AMERICA NORTH AMERICA ASIA AUSTRALIA ANTARCTICA INDIAN OCEAN PACIFIC ASIA AUSTRALIA ANTARCTICA INDIAN OCEAN PACIFIC OCEAN ATLANTIC OCEAN ARCTIC OCEAN SOUTHERN OCEAN AMERICA NORTH AMERICA ASIA AUSTRALIA ANTARCTICA INDIAN OCEAN PACIFIC OCEAN ATLANTIC OCEAN ARCTIC OCEAN

  19. Career Map: Instrumentation Coordinator

    Broader source: Energy.gov [DOE]

    The Wind Program's Career Map provides job description information for Instrumentation Coordinator positions.

  20. Oceans and Ecosystems Research Changing levels of Oceanic Carbon

    E-Print Network [OSTI]

    in the atmospheric, the remainder is taken up by land plants and oceans. · We study the uptake by the oceans both EPA qualified the increasing CO2 levels as a pollutant along with the other greenhouse gases Ch4, N2O & wind Algorithm development pCO2= f(SST, color) Co-located satellite data Regional satellite SST & color

  1. OCEAN PREDICTION WITH THE HYBRID COORDINATE OCEAN MODEL (HYCOM)

    E-Print Network [OSTI]

    . of South Florida, Fugro-GEOS, ROFFS, Orbimage, Shell, ExxonMobil #12;414 ERIC P. CHASSIGNET ET AL-resolving, real-time global and basin-scale ocean prediction system in the context of the Global Ocean Data Assimilation Experiment (GODAE). Keywords: HYCOM, GODAE, LAS, data assimilation, metrics. 1. Introduction

  2. Pacific Islands Fisheries Science Center Ecosystems and Oceanography Division

    E-Print Network [OSTI]

    Hawai'i at Manoa, University of

    Pacific Islands Fisheries Science Center Ecosystems and Oceanography Division Pelagic Fisheries Ecosystems and Oceanography Division Pacific Islands Fisheries Science Center, National Marine Fisheries and Oceanography Division Pelagic Fisheries Research Program Motivation · Juvenile & subadult bigeye aggregates

  3. Pacific Island Fisheries Science Center Ecosystems and Oceanography Division

    E-Print Network [OSTI]

    Hawai'i at Manoa, University of

    Pacific Island Fisheries Science Center Ecosystems and Oceanography Division Pelagic Fisheries Fisheries Science Center, NMFS, NOAA #12;Pacific Island Fisheries Science Center Ecosystems and Oceanography Science Center Ecosystems and Oceanography Division Pelagic Fisheries Research Program Materials

  4. MEASUREMENTS OF PAST 14C LEVELS AND 13C/12C RATIOS IN THE SURFACE WATERS OF THE WORLD'S SUBPOLAR OCEANS.

    SciTech Connect (OSTI)

    Brown, T A

    2010-04-22

    Under this project we have developed methods that allow the reconstruction of past {sup 14}C levels of the surface waters of the subpolar North Pacific Ocean by measuring the {sup 14}C contents of archived salmon scales. The overall goal of this research was to reduce of the uncertainty in the uptake of fossil CO{sub 2} by the oceans and thereby improve the quantification of the global carbon cycle and to elucidate the fate of anthropogenic CO{sub 2}. Ocean General Circulation Models (OGCMs), with their three dimensional global spatial coverage and temporal modeling capabilities, provide the best route to accurately calculating the total uptake of CO{sub 2} by the oceans and, hence, to achieving the desired reduction in uncertainty. {sup 14}C has played, and continues to play, a central role in the validation of the OGCMs calculations, particularly with respect to those model components which govern the uptake of CO{sub 2} from the atmosphere and the transport of this carbon within the oceans. Under this project, we have developed time-series records of the {sup 14}C levels of the surface waters of three areas of the subpolar North Pacific Ocean. As the previously available data on the time-history of oceanic surface water {sup 14}C levels are very limited, these time-series records provide significant new {sup 14}C data to constrain and validate the OGCMs.

  5. Coastal ocean margins program

    SciTech Connect (OSTI)

    Not Available

    1988-12-01

    The marine research program supported by the Office of Energy Research, Ecological Research Division, is focused to provide scientific information on major environmental issues facing development and expansion of most energy technologies and energy policy. These issues include waste disposal, siting/operations, and possible long term effects on global systems. The research is concentrated along the United States coastal margins where marine waters provide abundant food and resources while assimilating discharges from atmospheric, terrestrial, and aquatic sources. The program focuses on the formation and transport of particles within the waters of the continental shelf and the fate of these particles, whether on the shelf, on the slope, or in the open ocean. The program is conducted with multidisciplinary teams of researchers who investigate water mass movements, biological productivity, and naturally forming particles, as well as contaminant transport, to develop a clear understanding of the exchanges of contaminants and other materials that take place between continental shelf and open ocean waters. Seventy-five percent of the projects are funded to university grantees and twenty-five percent to National Laboratories.

  6. 2011 Annual Ecological Survey: Pacific Northwest National Laboratory Site

    SciTech Connect (OSTI)

    Becker, James M.; Chamness, Michele A.

    2012-02-27

    The U.S. Department of Energy (DOE) Pacific Northwest Site Office (PNSO) oversees and manages the DOE contract for the Pacific Northwest National Laboratory (PNNL), a DOE Office of Science multi-program laboratory located in Richland, Washington. PNSO is responsible for ensuring that all activities conducted on the PNNL site comply with applicable laws, policies, and DOE Orders. The DOE Pacific Northwest Site Office Cultural and Biological Resources Management Plan (DOE/PNSO 2008) addresses the requirement for annual surveys and monitoring for species of concern and to identify and map invasive species. In addition to the requirement for an annual survey, proposed project activities must be reviewed to assess any potential environmental consequences of conducting the project. The assessment process requires a thorough understanding of the resources present, the potential impacts of a proposed action to those resources, and the ultimate consequences of those actions. The PNNL site is situated on the southeastern corner of the DOE Hanford Site, located at the north end of the city of Richland in south-central Washington. The site is bordered on the east by the Columbia River, on the west by Stevens Drive, and on the north by the Hanford Site 300 Area (Figure 1). The environmental setting of the PNNL site is described in Larson and Downs (2009). There are currently two facilities on the PNNL site: the William R. Wiley Environmental Molecular Sciences Laboratory and the Physical Sciences Facility. This report describes the annual survey of biological resources found on the undeveloped upland portions of the PNNL site. The annual survey is comprised of a series of individual field surveys conducted on various days in late May and throughout June 2011. A brief description of the methods PNNL ecologists used to conduct the baseline surveys and a summary of the results of the surveys are presented. Appendix A provides a list of plant and animal species identified in the upland areas of the PNNL site in 2011. Efforts in 2011 to control noxious weed populations (comprising plant species designated as Class B noxious weeds by the Washington State Noxious Weed Control Board) discovered in 2009 and initially treated with herbicides in 2010 are described in Appendix B.

  7. Association of Pacific Rim Universities APRU Doctoral Student Conference

    E-Print Network [OSTI]

    Yamamoto, Hirosuke

    Association of Pacific Rim Universities (APRU) 6th APRU Doctoral Student Conference-discipline conference for doctoral students from different universities in Pacific Rim has been realized. Such global the Pacific Rim." It was the first time for the author to get feed back from and do interaction

  8. RESPONSES OF STREAM BIOFILM TO PACIFIC SALMON (ONCORHYNCHUS SPP.) SPAWNERS

    E-Print Network [OSTI]

    Lamberti, Gary A.

    Pacific Rim. The dynam- ics of salmon runs and environmental conditions of streams in which they spawn canRESPONSES OF STREAM BIOFILM TO PACIFIC SALMON (ONCORHYNCHUS SPP.) SPAWNERS: THE ROLE by Janine R¨uegg 2011 All Rights Reserved #12;RESPONSES OF STREAM BIOFILM TO PACIFIC SALMON (ONCORHYNCHUS

  9. Conference Report Annual Association of Pacific Rim Universities

    E-Print Network [OSTI]

    Yamamoto, Hirosuke

    Conference Report 9th Annual Association of Pacific Rim Universities Doctoral Student Conference in 1997, the Association of Pacific Rim Universities (APRU) is a consortium of 42 leading research://www.apru.org/about/members.htm) in the Pacific Rim. APRU aims to foster education, research and enterprise thereby contributing to the economic

  10. Association Pacific Rim Universities (APRU) Doctoral Students Conference

    E-Print Network [OSTI]

    Wu, Yih-Min

    The 12th Association Pacific Rim Universities (APRU) Doctoral Students Conference "Innovation: Fostering Sustainable Development and Harmony among Pacific Rim Communities" Call for Papers Tsinghua University (THU) is pleased to host the 12th Association of Pacific Rim Universities Doctoral Students

  11. Response of Juvenile Pacific Lamprey to Turbine Passage

    SciTech Connect (OSTI)

    Dauble, D.

    2009-09-14

    To help determine the Pacific lamprey’s ability to survive turbine passage, Pacific Northwest National Laboratory scientists conducted laboratory tests designed to simulate a fish’s passage through the turbine environment. Juvenile Pacific lamprey were subjected to two of three aspects of passage: pressure drop and shear stress. The third aspect, blade strike, was not tested.

  12. In Prince William Sound, Alaska, Pacific herring (Clupea pallasi) and

    E-Print Network [OSTI]

    400 In Prince William Sound, Alaska, Pacific herring (Clupea pallasi) and walleye pollock (Theragra the abundance of both these species in Prince William Sound has fluc- tuated, particularly that of Pacific) spatial distributions in Prince Wil- liam Sound, Alaska. We hypothe- sized that juvenile Pacific herring

  13. Modeling Ocean Ecosystems: The PARADIGM Program

    E-Print Network [OSTI]

    Rothstein, Lewis M.

    The role of the oceans in Earth systems ecology, and the effects of climate variability on the ocean and its ecosystems, can be understood only by observing, describing, and ultimately predicting the state of the ocean as ...

  14. Oceans and Human Health (and climate change)

    E-Print Network [OSTI]

    Zhou, Xianghong Jasmine

    Oceans and Human Health (and climate change) Tracy K. Collier Science Dimensions and Ocean Health in a Changing Climate, USC March 12, 2013 1 #12 use Climate change Closes the loop in understanding connections between ocean health and human health

  15. Marine Ecosystems Ocean Environment Research Division

    E-Print Network [OSTI]

    been studying how CO2 emissions affect the ocean system for more than three decades and conQnue to monitor ocean acidificaQon in all the world's oceans from

  16. HOW TO COOK OCEAN PERCH

    E-Print Network [OSTI]

    , is an excellent food fish with firm fle h. When cooked, the meat is white and flaky, with a delicate flavor. Ocean to the consumer until 1935. At that time, the indlu;try began experimenting with filleting and freezing ocean pel

  17. November 2002 OCEAN DRILLING PROGRAM

    E-Print Network [OSTI]

    November 2002 OCEAN DRILLING PROGRAM LEG 209 SCIENTIFIC PROSPECTUS DRILLING MANTLE PERIDOTITE ALONG Drilling Program Texas A&M University 1000 Discovery Drive College Station TX 77845-9547 USA -------------------------------- Dr. D. Jay Miller Leg Project Manager and Staff Scientist Ocean Drilling Program Texas A&M University

  18. January 2003 OCEAN DRILLING PROGRAM

    E-Print Network [OSTI]

    January 2003 OCEAN DRILLING PROGRAM LEG 210 SCIENTIFIC PROSPECTUS DRILLING THE NEWFOUNDLAND HALF OF THE NEWFOUNDLAND­IBERIA TRANSECT: THE FIRST CONJUGATE MARGIN DRILLING IN A NON-VOLCANIC RIFT Brian E. Tucholke Co Baldauf Deputy Director of Science Operations Ocean Drilling Program Texas A&M University 1000 Discovery

  19. Ocean Systems Lecture 16 & 17

    E-Print Network [OSTI]

    Richerson, Peter J.

    to thrive in oceans and lakes they need sunlight and nutrients. But thermal stratification tends to separateOcean Systems Lecture 16 & 17 #12;Hydroclimate, heat budgets and stratification For plants the nature of stratification. Light, less dense, water floats on top of colder, less dense water. Plankton

  20. 2010 Western Pacific Geophysics Search Results

    E-Print Network [OSTI]

    Ng, Chung-Sang

    2010 Western Pacific Geophysics Meeting Search Results Cite abstracts as Author(s) (2010), Title: Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, United States AU: Ragunathan, S EM: srivatta@gi.alaska.edu AF: Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, United

  1. Asian American and Pacific Islander Heritage Month

    Broader source: Energy.gov [DOE]

    A celebration of Asians and Pacific Islanders in the United States. The month of May was chosen to commemorate the immigration of the first Japanese to the United States on May 7, 1843, and to mark the anniversary of the completion of the transcontinental railroad on May 10, 1869. The majority of the workers who laid the tracks were Chinese immigrants.

  2. 2013Science Pacific Northwest National Laboratory (PNNL),

    E-Print Network [OSTI]

    2013Science Frontiers #12;Pacific Northwest National Laboratory (PNNL), a U.S. Department of Energy Office of Science Laboratory, is pushing the frontiers of science in areas that are critical to the nation's security, health and prosperity. PNNL's science and technology base ranges from basic research

  3. PACIFIC NORTHWEST ELECTRIC POWER PLANNING AND

    E-Print Network [OSTI]

    to energy conservation, renewable resources, other resources, and protecting, mitigating, and enhancing fish Stat.2697.] 839(1)(8). the development of renewable resources within the Pacific Northwest; [Northwest continue to pay all costs necessary to produce, transmit, and conserve resources to meet the region

  4. Ocean Surface Topography Mission/ Jason 2 Launch

    E-Print Network [OSTI]

    Ocean Surface Topography Mission/ Jason 2 Launch PreSS KiT/JUNe 2008 #12;#12;Media Contacts Steve .............................................................................................................................. 7 Why Study Ocean Surface Topography

  5. Iron Availability in the Southern Ocean

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Iron Availability in the Southern Ocean Print The Southern Ocean, circling the Earth between Antarctica and the southernmost regions of Africa, South America, and Australia, is...

  6. California Small Hydropower and Ocean Wave Energy

    E-Print Network [OSTI]

    California Small Hydropower and Ocean Wave Energy Resources IN SUPPORT OF THE 2005 INTEGRATED....................................................................................................................... 9 Ocean Wave Energy............................................................................................................. 20 Wave Energy Conversion Technology

  7. Ocean Power (4 Activities) | Department of Energy

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    our existing non-renewable resources. Ocean power is divided into three categories: wave energy, tidal energy, and ocean thermal energy conversion (OTEC) Systems. It is...

  8. Foraging ecology of North Pacific albacore in the California Current System

    E-Print Network [OSTI]

    Glaser, Sarah M.

    2009-01-01

    California Current System. California Cooperative OceanicCalifornia Current system. California Cooperative OceanicCalifornia Current region. California Cooperative Oceanic

  9. The export of carbon mediated by mesopelagic fishes in the northeast Pacific Ocean

    E-Print Network [OSTI]

    Davison, Peter Charles

    2011-01-01

    Randall, D.J. (Eds. ), Bioenergetics and growth. AcademicJobling, M. , 1993. Bioenergetics: feed intake and energy

  10. Decadal Variability in the Formation of the North Pacific Subtropical Mode Water: Oceanic versus Atmospheric Control

    E-Print Network [OSTI]

    Qiu, Bo

    , during which time high regional eddy variability infuses high-PV KE water into the recirculation gyre

  11. Distribution of phytoplankton pigments in the North Pacific Ocean in relation to optical and physical variability 

    E-Print Network [OSTI]

    Ondrusek, Michael Ernest

    1989-01-01

    microscopes, and generally confined to single classes of phytoplankton (i. e. , diatoms by VENRICK, 1971), or they have not been completely representative due to difficulty in preservation of the smaller, fragile forms (HASLE, 1959). TAKAHASHI and HORI...

  12. Pacific Ocean Pleistocene and Holocene surface temperature variability and implications for climate change

    E-Print Network [OSTI]

    Dyez, Kelsey

    2012-01-01

    is original and that diagenesis did not alter these samples.deposited, we assume that diagenesis may not be a factor

  13. A climatology of tropical moisture bursts in the eastern North Pacific Ocean 

    E-Print Network [OSTI]

    Smith, Neil Ray

    1986-01-01

    composited from the northbound orbital passes on the sun-lit half of the earth. The night IR is a composite of the southbound return passes on the dark side. Any feature observed by the satellite on a northbound pass, for example, will be observed again..., is obIectivelo def'ined ui terms of appearance m unenhanced IR satellite imagery as a continuous hand of upper, or middle arid upper, level clouds v;hich i? 2000 km in length and crosses 15'N. The de(in tion is pnmarily geometric and does...

  14. The export of carbon mediated by mesopelagic fishes in the northeast Pacific Ocean

    E-Print Network [OSTI]

    Davison, Peter Charles

    2011-01-01

    population migration and feeding at depth by VM fishes thatMigration, DVM). A portion of the DSL remains at depthdepth than it decreases blow 400 m, and because the effort of vertical migration

  15. Quaternary Science Reviews 21 (2002) 16931704 Interior hydrography and circulation of the glacial Pacific Ocean

    E-Print Network [OSTI]

    Lynch-Stieglitz, Jean

    2002-01-01

    has a large capacity to store heat and various dissolved species of gases and salts. In addition shorter than that for plate tectonics, the total surface carbon reservoir in the atmosphere

  16. Asian anthropogenic lead contamination in the North Pacific Ocean as evidenced by stable lead isotopic compositions

    E-Print Network [OSTI]

    Zurbrick, Cheryl Marie

    2014-01-01

    BY CURRENT AND PAST SOURCES OF CONTAMINATION ………. 85S. A. (1996) Metal contamination in San Francisco Bay2012) GEOTRACES IC1 (BATS) contamination-prone trace element

  17. Pacific Ocean Pleistocene and Holocene surface temperature variability and implications for climate change

    E-Print Network [OSTI]

    Dyez, Kelsey

    2012-01-01

    Mix et al. , 1999; Ostertag- Henning and Stax, 2000; SabinMix et al. , 1999; Ostertag-Henning and Stax, 2000; Sabin

  18. Atomic chlorine concentrations derived from ethane and hydroxyl measurements over the equatorial Pacific Ocean: Implication for

    E-Print Network [OSTI]

    Wingenter, Oliver W.

    Atomic chlorine concentrations derived from ethane and hydroxyl measurements over the equatorial model includes in situ observations of hydroxyl [HO] and precise measurements of ethane (C2H6) mixing ratios. Ethane was $40 pptv higher in the buffer layer (BuL) than in the SL, thus vertical exchange

  19. The export of carbon mediated by mesopelagic fishes in the northeast Pacific Ocean

    E-Print Network [OSTI]

    Davison, Peter Charles

    2011-01-01

    energy and materials in marine ecosystems. Plenum Press, Newenergy and materials in marine ecosystems. Plenum Press, Newenergy and materials in marine ecosystems. Plenum Press, New

  20. Increases in deep ocean ambient noise in the northeast pacific west of San Nicolas Island, California

    E-Print Network [OSTI]

    McDonald, M A; Hildebrand, John A; Wiggins, S M

    2006-01-01

    shelf. A nearby weather buoy gives detailed information on2003 at Tanner Bank ?NDBC buoy 46047?. The in?uence of windavailable from a National Data Buoy Center ?NDBC? weather

  1. Assessing the uncertainties of model estimates of primary productivity in the tropical Pacific Ocean

    E-Print Network [OSTI]

    2009-01-01

    Ciotti, A. , Dierssen, H. , Dowell, M. , Dunne, J. , Esaias,mark.dowell@jrc.it (M. Dowell), jpd@gfdl.noaa.gov (J.Scott C. Doney m , Mark Dowell n , John Dunne o , Bernard

  2. Asian anthropogenic lead contamination in the North Pacific Ocean as evidenced by stable lead isotopic compositions

    E-Print Network [OSTI]

    Zurbrick, Cheryl Marie

    2014-01-01

    analyses 3.7 dissolved Pb in offshore profiles dissolved Pb2). This cruise began offshore of Japan and had stations inand subsurface waters offshore, where the Kuroshio and

  3. Causes of Ocean Surface temperature Changes in Atlantic and Pacific Topical Cyclogenesis Regions

    E-Print Network [OSTI]

    2006-01-01

    17, 1777 (2004). 11. T. P. Barnett, D. W. Pierce, R. Schnur,267 (2001). 13. T. P. Barnett et al. , Science 309, 284 (4 K. AchutaRao, 1 T.P. Barnett, 5 J.S. Boyle, 1 W. Br¨

  4. Straddling 0 degreeS latitude in the eastern Pacific Ocean, the galpagos islands are extremely

    E-Print Network [OSTI]

    Sachs, Julian P.

    abundant rainfall to tropical islands. a fog layer, locally called `garúa' envelops the highlands the western part of the archipelago frequently brings thick sea fog lapping the arid shores of Fernandina penetrating saltwater intrusion around the whole coastal fringe. above the saltwater lies the freshwater lens

  5. The export of carbon mediated by mesopelagic fishes in the northeast Pacific Ocean

    E-Print Network [OSTI]

    Davison, Peter Charles

    2011-01-01

    Chapter 4. Carbon export mediated by mesopelagic fishes inLandry, M.R. , 2001. Active export of carbon and nitrogen atthat control particle export and flux attenuation in the

  6. Relationships between El Nino and the westerly winds in the South Pacific Ocean 

    E-Print Network [OSTI]

    Salva Pando, Antonio Jaime

    1976-01-01

    and similar phenomena in world weather. A modernized view of the Southern Oscillation, by Berlage and Boer (1959), is given in Fig. 4 and 5. Berlage (1966) associates the phenomenon with variations in solar activity and the turbidity of the atmosphere...

  7. Observed reflectivity of the western boundary of the equatorial Pacific Ocean

    E-Print Network [OSTI]

    Wunsch, Carl

    consistent with the Rossby wave and Kelvin wave dispersion relationship as the energy of Rossby wave-Lueng Fu Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA Carl Wunsch Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology

  8. Acoustic shadow-zone arrivals at long range in the North Pacific Ocean

    E-Print Network [OSTI]

    Van Uffelen, Lora J.

    2009-01-01

    with 1-GM internal-wave energy (right). The hor- izontal1-GM, and 2-GM internal-wave energy levels. . . . . FigureGarrett-Munk internal-wave energy spectrum at full strength

  9. Acoustic shadow-zone arrivals at long range in the North Pacific Ocean

    E-Print Network [OSTI]

    Van Uffelen, Lora J.

    2009-01-01

    with 1-GM internal-wave energy (right). The hor- izontal1-GM, and 2-GM internal-wave energy levels. . . . . Figurethe Garrett-Munk internal-wave energy spectrum (right), and

  10. MICRONEKTON OF THE EASTERN TROPICAL PACIFIC OCEAN: FAMILY COMPOSITION, DISTRIBUTION, ABUNDANCE, AND RELATIONS TO

    E-Print Network [OSTI]

    pelamis) from the same areas; agreement between catches and stomach samples was fair for crustaceans

  11. Distributions of crenarchaeal amoA genes and transcripts in the Pacific Ocean

    E-Print Network [OSTI]

    Church, Matthew J.

    Planktonic Crenarchaea are thought to play a key role in chemolithotrophic ammonia oxidation, a critical step of the marine nitrogen (N) cycle. In this study, we examined the spatial distributions of ammonia-oxidizing ...

  12. Distal transport of dissolved hydrothermal iron in the deep South Pacific Ocean

    E-Print Network [OSTI]

    Fitzsimmons, Jessica N.

    Until recently, hydrothermal vents were not considered to be an important source to the marine dissolved Fe (dFe) inventory because hydrothermal Fe was believed to precipitate quantitatively near the vent site. Based on ...

  13. Understanding the Regional Variability of Eddy Diffusivity in the Pacific Sector of the Southern Ocean

    E-Print Network [OSTI]

    Shuckburgh, Emily

    A diagnostic framework is presented, based on the Nakamura effective diffusivity, to investigate the regional variation in eddy diffusivity. Comparison of three different diffusivity calculations enables the effects of ...

  14. The export of carbon mediated by mesopelagic fishes in the northeast Pacific Ocean

    E-Print Network [OSTI]

    Davison, Peter Charles

    2011-01-01

    Ed. ), Flows of energy and materials in marine ecosystems.Ed. ), Flows of energy and materials in marine ecosystems.Ed. ), Flows of energy and materials in marine ecosystems,

  15. The North Pacific subtropical gyre is a large oceanic gyre bounded on

    E-Print Network [OSTI]

    Hawai'i at Manoa, University of

    /index.php) to investigate whether the ecosystem contained any keystone species (Kitchell et al., 1999; 2002). The results indicated that there was not any single species group that func- tioned as a keystone, but that a broad; 2002). In effect, the fishing fleet is the keystone preda- tor (Kitchell et al., 1999). However another

  16. Acoustic shadow-zone arrivals at long range in the North Pacific Ocean

    E-Print Network [OSTI]

    Van Uffelen, Lora J.

    2009-01-01

    1-GM internal-wave energy (right). The hor- izontal linesinternal-wave energy spectrum (right), and an incoherentinternal-wave energy spectrum (right), and an incoherent

  17. Establishing a Testing Center for Ocean Energy Technologies in the Pacific

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home Page on Delicious Rank EERE: Alternative Fuelsof Energy Services » Program Management »Eric J. Fygi About Us Eric

  18. "Towards Optics-Based Measurements in Ocean Observatories"

    E-Print Network [OSTI]

    Boss, Emmanuel S.

    /JPSS ­ UAV ­ Ocean optics, Biological ­ Laser penetration New opportunity · Insitu Sensors ­ (Gliders"Towards Optics-Based Measurements in Ocean Observatories" "Ocean Observatories Contributions to Ocean Models and Data Assimilation For Ecosystems" Ocean Optics 2012 Glasgow Scotland Robert Arnone

  19. The Ocean Sampling Day Consortium

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Kopf, Anna; Bicak, Mesude; Kottmann, Renzo; Schnetzer, Julia; Kostadinov, Ivaylo; Lehmann, Katja; Fernandez-Guerra, Antonio; Jeanthon, Christian; Rahav, Eyal; Ullrich, Matthias; et al

    2015-06-19

    In this study, Ocean Sampling Day was initiated by the EU-funded Micro B3 (Marine Microbial Biodiversity, Bioinformatics, Biotechnology) project to obtain a snapshot of the marine microbial biodiversity and function of the world’s oceans. It is a simultaneous global mega-sequencing campaign aiming to generate the largest standardized microbial data set in a single day. This will be achievable only through the coordinated efforts of an Ocean Sampling Day Consortium, supportive partnerships and networks between sites. This commentary outlines the establishment, function and aims of the Consortium and describes our vision for a sustainable study of marine microbial communities and theirmore »embedded functional traits.« less

  20. Introgression & mapping Fiber cell

    E-Print Network [OSTI]

    Germplasm Introgression Genomics & mapping Fiber cell initiation Radiation hybrid (RH) mapping and breeding. Research activities commonly include plant breeding, genetics, genomics, cytogenetics, molecular methods. (C, S) · Contribute uniquely to genomics and its relevance to genetic improvement (C,S) · Harness

  1. SERC Grants Interactive Map

    Broader source: Energy.gov [DOE]

    View SERC Grants in a larger map. To report corrections, please email SustainableEnergyWAP@ee.doe.gov.

  2. National Hydropower Map

    Broader source: Energy.gov [DOE]

    High-resolution map produced by Oak Ridge National Laboratory showing hydropower resources throughout the United States.

  3. WIPP Projects Interative Map

    Broader source: Energy.gov [DOE]

    View WIPP Projects in a larger map. To report corrections, please email WeatherizationInnovation@ee.doe.gov.

  4. Flood Inundation Mapping

    E-Print Network [OSTI]

    Pearson, Wendy

    2009-11-18

    for Life Decisions” Page 16 Inundation Mapping Activities There are considerable interests across many parts of Central Region. Central Indiana Partnership among NOAA, USGS, Polis Center, and Indiana to develop near real-time inundation maps based... for Life Decisions” Page 16 Inundation Mapping Activities There are considerable interests across many parts of Central Region. Central Indiana Partnership among NOAA, USGS, Polis Center, and Indiana to develop near real-time inundation maps based...

  5. OUTLINE OF DATA SOURCES, MAY 1933 LANDAREAS OCEAN AREAS SOURCES OF DATA

    E-Print Network [OSTI]

    ~ecldeallydv- en.but when Drmnt weather is rewrted: Base map descdptIon N used when coverage mbsing "round i#12;#12;#12;OUTLINE OF DATA SOURCES, MAY 1933 LANDAREAS OCEAN AREAS SOURCES OF DATA Area Bource National dfdeordogiguc dc Efance. 2 Daily Weather Report, Egypt. 3 Monthly Meteorological Bulletin, Nanking

  6. Evaluating carbon sequestration efficiency in an ocean circulation model by adjoint sensitivity analysis

    E-Print Network [OSTI]

    Follows, Mick

    Evaluating carbon sequestration efficiency in an ocean circulation model by adjoint sensitivity the application of the adjoint method to develop three-dimensional maps of carbon sequestration efficiency. Sequestration efficiency (the percentage of carbon injected at a continuous point source that remains

  7. Modeling of tsunami sources and propagation in the Atlantic Ocean Basin to assess coastal tsunami

    E-Print Network [OSTI]

    Kirby, James T.

    Modeling of tsunami sources and propagation in the Atlantic Ocean Basin to assess coastal tsunami 19716, USA Abstract Since 2010, under the auspices of the US National Tsunami Hazard Mitigation Pro- gram (NTHMP), the authors have conducted modeling work to gradually develop tsunami inundation maps

  8. Curriculum Mapping . 1 .../...

    E-Print Network [OSTI]

    Laksanacharoen, Sathaporn

    #12; TQF ­ #12; / . 5 / #12; 5 #12;Curriculum Mapping #12 ( (Curriculum Mapping) 1) 2) 1 3) ) #12; 1. - - - - - - - - #12. - - - - - - - - - - 0.3 - Power- point - .. #12;2. ( (CurriculumMapping) ) * 1.4, 1.5 2.2, 2.3, 2.6 3

  9. Historical Maps Online 

    E-Print Network [OSTI]

    Rumsey, David Y.

    2005-01-31

    ://www.davidrumsey.com/, which currently has over 10,000 high resolution images of maps from his collection. He has also built a suite of tools for users to experience and interpret the maps online. These include GIS, which allows users to combine historical maps with modern...

  10. The Link Foundation Ocean Engineering and Instrumentation

    E-Print Network [OSTI]

    Virginia Tech

    and ocean instrumentation. Application Available online at www.linkoe.org or write to/email: Forms and DrThe Link Foundation Ocean Engineering and Instrumentation Ph.D. Fellowship Program Objectives: To foster ocean engineering and ocean instrumentation research; to enhance both the theoretical

  11. Response of photosynthesis to ocean acidification

    E-Print Network [OSTI]

    Mackey, KRM; Morris, JJ; Morris, JJ; Morel, FMM; Kranz, SA

    2015-01-01

    primary productiv- ity, especially in the oligotrophic regions of the ocean. In addition to the energy

  12. OCEAN DRILLING PROGRAM LEG 165 SCIENTIFIC PROSPECTUS

    E-Print Network [OSTI]

    OCEAN DRILLING PROGRAM LEG 165 SCIENTIFIC PROSPECTUS CARIBBEAN OCEAN HISTORY AND THE CRETACEOUS Scientist, Leg 165 Ocean Drilling Program Texas A&M University Research Park 1000 Discovery Drive College of any portion requires the written consent of the Director, Ocean Drilling Program, Texas A&M University

  13. OCEAN DRILLING PROGRAM LEG 110 SCIENTIFIC PROSPECTUS

    E-Print Network [OSTI]

    OCEAN DRILLING PROGRAM LEG 110 SCIENTIFIC PROSPECTUS LESSER ANTILLES FOREARC J. Casey Moore Staff Science Representative, Leg 110 Ocean Drilling Program Texas A&M University College Station, TX 77843-3469 Philip D. Direct* Ocean Drilling Program Robert B. Kidd Manager of Science Operations Ocean

  14. INSTRUCTIONS INTEGRATED OCEAN DRILLING PROGRAM (IODP)

    E-Print Network [OSTI]

    INSTRUCTIONS FOR THE INTEGRATED OCEAN DRILLING PROGRAM (IODP) MANUSCRIPT AND PHOTOGRAPH COPYRIGHT, Integrated Ocean Drilling Program, 1000 Discovery Drive, College Station, Texas 77845, USA A signed copyright of the Integrated Ocean Drilling Program or any other publications of the Integrated Ocean Drilling Program. Author

  15. OCEAN DRILLING PROGRAM LEG 109 PRELIMINARY REPORT

    E-Print Network [OSTI]

    OCEAN DRILLING PROGRAM LEG 109 PRELIMINARY REPORT BARE ROCK DRILLING IN THE MID-ATLANTIC RIDGE RIFT 109 Ocean Drilling Program Texas A & M University College Station, TX 77843-3469 Philip D. Rabinowitz Director Ocean Drilling Program Robert B. Kidd Manager of Science Operations Ocean Drilling Program Louis E

  16. OCEAN DRILLING PROGRAM LEG 104 SCIENTIFIC PROSPECTUS

    E-Print Network [OSTI]

    OCEAN DRILLING PROGRAM LEG 104 SCIENTIFIC PROSPECTUS NORWEGIAN SEA Olav Eldholm Co-Chief Scientist Ocean Drilling Program Texas A & M University College Station, Texas 77843-3469 Pni±ip o Rabinowitz Director Ocean Drilling Program Robert B Kidd Manager of Science Operations Ocean Drilling Program Louis E

  17. WORLD OCEAN ATLAS 2013 Product Documentation

    E-Print Network [OSTI]

    WORLD OCEAN ATLAS 2013 Product Documentation Ocean Climate Laboratory NODC / NESDIS / NOAA Silver: World Ocean Atlas 2013 Product Documentation. T. Boyer, Ed.; A. Mishonov, Technical Ed.; 14 pp such as mixed layer depth. Upon publishing Climatological Atlas of the World Ocean in 1982, he distributed

  18. Newsletter of Coastal Ocean Processes

    E-Print Network [OSTI]

    Science Workshop Executive Summary Draft OCEAN.US Airlie House Workshop Update Evolution of the Cross and the following working groups: 1.Trace elements in ecological and biogeochemical processes 2.Physical forcing

  19. Mercury in the Anthropocene Ocean

    E-Print Network [OSTI]

    Lamborg, Carl

    The toxic metal mercury is present only at trace levels in the ocean, but it accumulates in fish at concentrations high enough to pose a threat to human and environmental health. Human activity has dramatically altered the ...

  20. Ocean Renewable Energy Conference X

    Broader source: Energy.gov [DOE]

    The 10th annual Ocean Renewable Energy Conference provides attendees a forum to share new ideas and concepts, opportunity to learn from leading-edge practitioners and policy-makers, information...